Deprecated (16384): The ArrayAccess methods will be removed in 4.0.0.Use getParam(), getData() and getQuery() instead. - /home/brlfuser/public_html/src/Controller/ArtileDetailController.php, line: 73 You can disable deprecation warnings by setting `Error.errorLevel` to `E_ALL & ~E_USER_DEPRECATED` in your config/app.php. [CORE/src/Core/functions.php, line 311]Code Context
trigger_error($message, E_USER_DEPRECATED);
}
$message = 'The ArrayAccess methods will be removed in 4.0.0.Use getParam(), getData() and getQuery() instead. - /home/brlfuser/public_html/src/Controller/ArtileDetailController.php, line: 73 You can disable deprecation warnings by setting `Error.errorLevel` to `E_ALL & ~E_USER_DEPRECATED` in your config/app.php.' $stackFrame = (int) 1 $trace = [ (int) 0 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/ServerRequest.php', 'line' => (int) 2421, 'function' => 'deprecationWarning', 'args' => [ (int) 0 => 'The ArrayAccess methods will be removed in 4.0.0.Use getParam(), getData() and getQuery() instead.' ] ], (int) 1 => [ 'file' => '/home/brlfuser/public_html/src/Controller/ArtileDetailController.php', 'line' => (int) 73, 'function' => 'offsetGet', 'class' => 'Cake\Http\ServerRequest', 'object' => object(Cake\Http\ServerRequest) {}, 'type' => '->', 'args' => [ (int) 0 => 'catslug' ] ], (int) 2 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Controller/Controller.php', 'line' => (int) 610, 'function' => 'printArticle', 'class' => 'App\Controller\ArtileDetailController', 'object' => object(App\Controller\ArtileDetailController) {}, 'type' => '->', 'args' => [] ], (int) 3 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/ActionDispatcher.php', 'line' => (int) 120, 'function' => 'invokeAction', 'class' => 'Cake\Controller\Controller', 'object' => object(App\Controller\ArtileDetailController) {}, 'type' => '->', 'args' => [] ], (int) 4 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/ActionDispatcher.php', 'line' => (int) 94, 'function' => '_invoke', 'class' => 'Cake\Http\ActionDispatcher', 'object' => object(Cake\Http\ActionDispatcher) {}, 'type' => '->', 'args' => [ (int) 0 => object(App\Controller\ArtileDetailController) {} ] ], (int) 5 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/BaseApplication.php', 'line' => (int) 235, 'function' => 'dispatch', 'class' => 'Cake\Http\ActionDispatcher', 'object' => object(Cake\Http\ActionDispatcher) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {} ] ], (int) 6 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/Runner.php', 'line' => (int) 65, 'function' => '__invoke', 'class' => 'Cake\Http\BaseApplication', 'object' => object(App\Application) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {}, (int) 2 => object(Cake\Http\Runner) {} ] ], (int) 7 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Routing/Middleware/RoutingMiddleware.php', 'line' => (int) 162, 'function' => '__invoke', 'class' => 'Cake\Http\Runner', 'object' => object(Cake\Http\Runner) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {} ] ], (int) 8 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/Runner.php', 'line' => (int) 65, 'function' => '__invoke', 'class' => 'Cake\Routing\Middleware\RoutingMiddleware', 'object' => object(Cake\Routing\Middleware\RoutingMiddleware) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {}, (int) 2 => object(Cake\Http\Runner) {} ] ], (int) 9 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Routing/Middleware/AssetMiddleware.php', 'line' => (int) 88, 'function' => '__invoke', 'class' => 'Cake\Http\Runner', 'object' => object(Cake\Http\Runner) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {} ] ], (int) 10 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/Runner.php', 'line' => (int) 65, 'function' => '__invoke', 'class' => 'Cake\Routing\Middleware\AssetMiddleware', 'object' => object(Cake\Routing\Middleware\AssetMiddleware) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {}, (int) 2 => object(Cake\Http\Runner) {} ] ], (int) 11 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Error/Middleware/ErrorHandlerMiddleware.php', 'line' => (int) 96, 'function' => '__invoke', 'class' => 'Cake\Http\Runner', 'object' => object(Cake\Http\Runner) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {} ] ], (int) 12 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/Runner.php', 'line' => (int) 65, 'function' => '__invoke', 'class' => 'Cake\Error\Middleware\ErrorHandlerMiddleware', 'object' => object(Cake\Error\Middleware\ErrorHandlerMiddleware) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {}, (int) 2 => object(Cake\Http\Runner) {} ] ], (int) 13 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/Runner.php', 'line' => (int) 51, 'function' => '__invoke', 'class' => 'Cake\Http\Runner', 'object' => object(Cake\Http\Runner) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {} ] ], (int) 14 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/Server.php', 'line' => (int) 98, 'function' => 'run', 'class' => 'Cake\Http\Runner', 'object' => object(Cake\Http\Runner) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\MiddlewareQueue) {}, (int) 1 => object(Cake\Http\ServerRequest) {}, (int) 2 => object(Cake\Http\Response) {} ] ], (int) 15 => [ 'file' => '/home/brlfuser/public_html/webroot/index.php', 'line' => (int) 39, 'function' => 'run', 'class' => 'Cake\Http\Server', 'object' => object(Cake\Http\Server) {}, 'type' => '->', 'args' => [] ] ] $frame = [ 'file' => '/home/brlfuser/public_html/src/Controller/ArtileDetailController.php', 'line' => (int) 73, 'function' => 'offsetGet', 'class' => 'Cake\Http\ServerRequest', 'object' => object(Cake\Http\ServerRequest) { trustProxy => false [protected] params => [ [maximum depth reached] ] [protected] data => [[maximum depth reached]] [protected] query => [[maximum depth reached]] [protected] cookies => [ [maximum depth reached] ] [protected] _environment => [ [maximum depth reached] ] [protected] url => 'latest-news-updates/a-race-towards-climate-catastrophe-nagraj-adve-21393/print' [protected] base => '' [protected] webroot => '/' [protected] here => '/latest-news-updates/a-race-towards-climate-catastrophe-nagraj-adve-21393/print' [protected] trustedProxies => [[maximum depth reached]] [protected] _input => null [protected] _detectors => [ [maximum depth reached] ] [protected] _detectorCache => [ [maximum depth reached] ] [protected] stream => object(Zend\Diactoros\PhpInputStream) {} [protected] uri => object(Zend\Diactoros\Uri) {} [protected] session => object(Cake\Http\Session) {} [protected] attributes => [[maximum depth reached]] [protected] emulatedAttributes => [ [maximum depth reached] ] [protected] uploadedFiles => [[maximum depth reached]] [protected] protocol => null [protected] requestTarget => null [private] deprecatedProperties => [ [maximum depth reached] ] }, 'type' => '->', 'args' => [ (int) 0 => 'catslug' ] ]deprecationWarning - CORE/src/Core/functions.php, line 311 Cake\Http\ServerRequest::offsetGet() - CORE/src/Http/ServerRequest.php, line 2421 App\Controller\ArtileDetailController::printArticle() - APP/Controller/ArtileDetailController.php, line 73 Cake\Controller\Controller::invokeAction() - CORE/src/Controller/Controller.php, line 610 Cake\Http\ActionDispatcher::_invoke() - CORE/src/Http/ActionDispatcher.php, line 120 Cake\Http\ActionDispatcher::dispatch() - CORE/src/Http/ActionDispatcher.php, line 94 Cake\Http\BaseApplication::__invoke() - CORE/src/Http/BaseApplication.php, line 235 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Routing\Middleware\RoutingMiddleware::__invoke() - CORE/src/Routing/Middleware/RoutingMiddleware.php, line 162 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Routing\Middleware\AssetMiddleware::__invoke() - CORE/src/Routing/Middleware/AssetMiddleware.php, line 88 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Error\Middleware\ErrorHandlerMiddleware::__invoke() - CORE/src/Error/Middleware/ErrorHandlerMiddleware.php, line 96 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Http\Runner::run() - CORE/src/Http/Runner.php, line 51 Cake\Http\Server::run() - CORE/src/Http/Server.php, line 98
Deprecated (16384): The ArrayAccess methods will be removed in 4.0.0.Use getParam(), getData() and getQuery() instead. - /home/brlfuser/public_html/src/Controller/ArtileDetailController.php, line: 74 You can disable deprecation warnings by setting `Error.errorLevel` to `E_ALL & ~E_USER_DEPRECATED` in your config/app.php. [CORE/src/Core/functions.php, line 311]Code Context
trigger_error($message, E_USER_DEPRECATED);
}
$message = 'The ArrayAccess methods will be removed in 4.0.0.Use getParam(), getData() and getQuery() instead. - /home/brlfuser/public_html/src/Controller/ArtileDetailController.php, line: 74 You can disable deprecation warnings by setting `Error.errorLevel` to `E_ALL & ~E_USER_DEPRECATED` in your config/app.php.' $stackFrame = (int) 1 $trace = [ (int) 0 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/ServerRequest.php', 'line' => (int) 2421, 'function' => 'deprecationWarning', 'args' => [ (int) 0 => 'The ArrayAccess methods will be removed in 4.0.0.Use getParam(), getData() and getQuery() instead.' ] ], (int) 1 => [ 'file' => '/home/brlfuser/public_html/src/Controller/ArtileDetailController.php', 'line' => (int) 74, 'function' => 'offsetGet', 'class' => 'Cake\Http\ServerRequest', 'object' => object(Cake\Http\ServerRequest) {}, 'type' => '->', 'args' => [ (int) 0 => 'artileslug' ] ], (int) 2 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Controller/Controller.php', 'line' => (int) 610, 'function' => 'printArticle', 'class' => 'App\Controller\ArtileDetailController', 'object' => object(App\Controller\ArtileDetailController) {}, 'type' => '->', 'args' => [] ], (int) 3 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/ActionDispatcher.php', 'line' => (int) 120, 'function' => 'invokeAction', 'class' => 'Cake\Controller\Controller', 'object' => object(App\Controller\ArtileDetailController) {}, 'type' => '->', 'args' => [] ], (int) 4 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/ActionDispatcher.php', 'line' => (int) 94, 'function' => '_invoke', 'class' => 'Cake\Http\ActionDispatcher', 'object' => object(Cake\Http\ActionDispatcher) {}, 'type' => '->', 'args' => [ (int) 0 => object(App\Controller\ArtileDetailController) {} ] ], (int) 5 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/BaseApplication.php', 'line' => (int) 235, 'function' => 'dispatch', 'class' => 'Cake\Http\ActionDispatcher', 'object' => object(Cake\Http\ActionDispatcher) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {} ] ], (int) 6 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/Runner.php', 'line' => (int) 65, 'function' => '__invoke', 'class' => 'Cake\Http\BaseApplication', 'object' => object(App\Application) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {}, (int) 2 => object(Cake\Http\Runner) {} ] ], (int) 7 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Routing/Middleware/RoutingMiddleware.php', 'line' => (int) 162, 'function' => '__invoke', 'class' => 'Cake\Http\Runner', 'object' => object(Cake\Http\Runner) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {} ] ], (int) 8 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/Runner.php', 'line' => (int) 65, 'function' => '__invoke', 'class' => 'Cake\Routing\Middleware\RoutingMiddleware', 'object' => object(Cake\Routing\Middleware\RoutingMiddleware) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {}, (int) 2 => object(Cake\Http\Runner) {} ] ], (int) 9 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Routing/Middleware/AssetMiddleware.php', 'line' => (int) 88, 'function' => '__invoke', 'class' => 'Cake\Http\Runner', 'object' => object(Cake\Http\Runner) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {} ] ], (int) 10 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/Runner.php', 'line' => (int) 65, 'function' => '__invoke', 'class' => 'Cake\Routing\Middleware\AssetMiddleware', 'object' => object(Cake\Routing\Middleware\AssetMiddleware) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {}, (int) 2 => object(Cake\Http\Runner) {} ] ], (int) 11 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Error/Middleware/ErrorHandlerMiddleware.php', 'line' => (int) 96, 'function' => '__invoke', 'class' => 'Cake\Http\Runner', 'object' => object(Cake\Http\Runner) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {} ] ], (int) 12 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/Runner.php', 'line' => (int) 65, 'function' => '__invoke', 'class' => 'Cake\Error\Middleware\ErrorHandlerMiddleware', 'object' => object(Cake\Error\Middleware\ErrorHandlerMiddleware) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {}, (int) 2 => object(Cake\Http\Runner) {} ] ], (int) 13 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/Runner.php', 'line' => (int) 51, 'function' => '__invoke', 'class' => 'Cake\Http\Runner', 'object' => object(Cake\Http\Runner) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\ServerRequest) {}, (int) 1 => object(Cake\Http\Response) {} ] ], (int) 14 => [ 'file' => '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Http/Server.php', 'line' => (int) 98, 'function' => 'run', 'class' => 'Cake\Http\Runner', 'object' => object(Cake\Http\Runner) {}, 'type' => '->', 'args' => [ (int) 0 => object(Cake\Http\MiddlewareQueue) {}, (int) 1 => object(Cake\Http\ServerRequest) {}, (int) 2 => object(Cake\Http\Response) {} ] ], (int) 15 => [ 'file' => '/home/brlfuser/public_html/webroot/index.php', 'line' => (int) 39, 'function' => 'run', 'class' => 'Cake\Http\Server', 'object' => object(Cake\Http\Server) {}, 'type' => '->', 'args' => [] ] ] $frame = [ 'file' => '/home/brlfuser/public_html/src/Controller/ArtileDetailController.php', 'line' => (int) 74, 'function' => 'offsetGet', 'class' => 'Cake\Http\ServerRequest', 'object' => object(Cake\Http\ServerRequest) { trustProxy => false [protected] params => [ [maximum depth reached] ] [protected] data => [[maximum depth reached]] [protected] query => [[maximum depth reached]] [protected] cookies => [ [maximum depth reached] ] [protected] _environment => [ [maximum depth reached] ] [protected] url => 'latest-news-updates/a-race-towards-climate-catastrophe-nagraj-adve-21393/print' [protected] base => '' [protected] webroot => '/' [protected] here => '/latest-news-updates/a-race-towards-climate-catastrophe-nagraj-adve-21393/print' [protected] trustedProxies => [[maximum depth reached]] [protected] _input => null [protected] _detectors => [ [maximum depth reached] ] [protected] _detectorCache => [ [maximum depth reached] ] [protected] stream => object(Zend\Diactoros\PhpInputStream) {} [protected] uri => object(Zend\Diactoros\Uri) {} [protected] session => object(Cake\Http\Session) {} [protected] attributes => [[maximum depth reached]] [protected] emulatedAttributes => [ [maximum depth reached] ] [protected] uploadedFiles => [[maximum depth reached]] [protected] protocol => null [protected] requestTarget => null [private] deprecatedProperties => [ [maximum depth reached] ] }, 'type' => '->', 'args' => [ (int) 0 => 'artileslug' ] ]deprecationWarning - CORE/src/Core/functions.php, line 311 Cake\Http\ServerRequest::offsetGet() - CORE/src/Http/ServerRequest.php, line 2421 App\Controller\ArtileDetailController::printArticle() - APP/Controller/ArtileDetailController.php, line 74 Cake\Controller\Controller::invokeAction() - CORE/src/Controller/Controller.php, line 610 Cake\Http\ActionDispatcher::_invoke() - CORE/src/Http/ActionDispatcher.php, line 120 Cake\Http\ActionDispatcher::dispatch() - CORE/src/Http/ActionDispatcher.php, line 94 Cake\Http\BaseApplication::__invoke() - CORE/src/Http/BaseApplication.php, line 235 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Routing\Middleware\RoutingMiddleware::__invoke() - CORE/src/Routing/Middleware/RoutingMiddleware.php, line 162 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Routing\Middleware\AssetMiddleware::__invoke() - CORE/src/Routing/Middleware/AssetMiddleware.php, line 88 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Error\Middleware\ErrorHandlerMiddleware::__invoke() - CORE/src/Error/Middleware/ErrorHandlerMiddleware.php, line 96 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Http\Runner::run() - CORE/src/Http/Runner.php, line 51 Cake\Http\Server::run() - CORE/src/Http/Server.php, line 98
Warning (512): Unable to emit headers. Headers sent in file=/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Error/Debugger.php line=853 [CORE/src/Http/ResponseEmitter.php, line 48]Code Contextif (Configure::read('debug')) {
trigger_error($message, E_USER_WARNING);
} else {
$response = object(Cake\Http\Response) { 'status' => (int) 200, 'contentType' => 'text/html', 'headers' => [ 'Content-Type' => [ [maximum depth reached] ] ], 'file' => null, 'fileRange' => [], 'cookies' => object(Cake\Http\Cookie\CookieCollection) {}, 'cacheDirectives' => [], 'body' => '<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Transitional//EN" "http://www.w3.org/TR/xhtml1/DTD/xhtml1-transitional.dtd"> <html xmlns="http://www.w3.org/1999/xhtml"> <head> <link rel="canonical" href="https://im4change.in/<pre class="cake-error"><a href="javascript:void(0);" onclick="document.getElementById('cakeErr68035bdbe069d-trace').style.display = (document.getElementById('cakeErr68035bdbe069d-trace').style.display == 'none' ? '' : 'none');"><b>Notice</b> (8)</a>: Undefined variable: urlPrefix [<b>APP/Template/Layout/printlayout.ctp</b>, line <b>8</b>]<div id="cakeErr68035bdbe069d-trace" class="cake-stack-trace" style="display: none;"><a href="javascript:void(0);" onclick="document.getElementById('cakeErr68035bdbe069d-code').style.display = (document.getElementById('cakeErr68035bdbe069d-code').style.display == 'none' ? '' : 'none')">Code</a> <a href="javascript:void(0);" onclick="document.getElementById('cakeErr68035bdbe069d-context').style.display = (document.getElementById('cakeErr68035bdbe069d-context').style.display == 'none' ? '' : 'none')">Context</a><pre id="cakeErr68035bdbe069d-code" class="cake-code-dump" style="display: none;"><code><span style="color: #000000"><span style="color: #0000BB"></span><span style="color: #007700"><</span><span style="color: #0000BB">head</span><span style="color: #007700">> </span></span></code> <span class="code-highlight"><code><span style="color: #000000"> <link rel="canonical" href="<span style="color: #0000BB"><?php </span><span style="color: #007700">echo </span><span style="color: #0000BB">Configure</span><span style="color: #007700">::</span><span style="color: #0000BB">read</span><span style="color: #007700">(</span><span style="color: #DD0000">'SITE_URL'</span><span style="color: #007700">); </span><span style="color: #0000BB">?><?php </span><span style="color: #007700">echo </span><span style="color: #0000BB">$urlPrefix</span><span style="color: #007700">;</span><span style="color: #0000BB">?><?php </span><span style="color: #007700">echo </span><span style="color: #0000BB">$article_current</span><span style="color: #007700">-></span><span style="color: #0000BB">category</span><span style="color: #007700">-></span><span style="color: #0000BB">slug</span><span style="color: #007700">; </span><span style="color: #0000BB">?></span>/<span style="color: #0000BB"><?php </span><span style="color: #007700">echo </span><span style="color: #0000BB">$article_current</span><span style="color: #007700">-></span><span style="color: #0000BB">seo_url</span><span style="color: #007700">; </span><span style="color: #0000BB">?></span>.html"/> </span></code></span> <code><span style="color: #000000"><span style="color: #0000BB"> </span><span style="color: #007700"><</span><span style="color: #0000BB">meta http</span><span style="color: #007700">-</span><span style="color: #0000BB">equiv</span><span style="color: #007700">=</span><span style="color: #DD0000">"Content-Type" </span><span style="color: #0000BB">content</span><span style="color: #007700">=</span><span style="color: #DD0000">"text/html; charset=utf-8"</span><span style="color: #007700">/> </span></span></code></pre><pre id="cakeErr68035bdbe069d-context" class="cake-context" style="display: none;">$viewFile = '/home/brlfuser/public_html/src/Template/Layout/printlayout.ctp' $dataForView = [ 'article_current' => object(App\Model\Entity\Article) { 'id' => (int) 21248, 'title' => 'A race towards climate catastrophe-Nagraj Adve', 'subheading' => '', 'description' => '<div align="justify"> -The Hindu </div> <p align="justify"> &nbsp; </p> <p align="justify"> &nbsp; </p> <p align="justify"> <em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em> </p> <p align="justify"> When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons. </p> <p align="justify"> <em>Impact on life cycles</em> </p> <p align="justify"> One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade. </p> <p align="justify"> This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species. </p> <p align="justify"> This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or &quot;been the first groups in which whole species have gone extinct due to recent climate change.&quot; </p> <p align="justify"> Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that &quot;if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that&quot; (&quot;Target Atmospheric CO: Where Should Humanity Aim?,&quot; The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org. </p> <p align="justify"> <em>Temperature regulator</em> </p> <p align="justify"> Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: &quot;The similarity between CO and temperature in [the] Antarctica is jaw-dropping,&quot; a causal link he says that's even stronger than that between smoking and lung cancer, &quot;kind of a gold standard in the medical world.&quot; Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience. </p> <p align="justify"> We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop. </p> <p align="justify"> <em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em> </p>', 'credit_writer' => 'The Hindu, 4 June, 2013, http://www.thehindu.com/opinion/op-ed/a-race-towards-climate-catastrophe/article4778996.ece', 'article_img' => '', 'article_img_thumb' => '', 'status' => (int) 1, 'show_on_home' => (int) 1, 'lang' => 'EN', 'category_id' => (int) 16, 'tag_keyword' => '', 'seo_url' => 'a-race-towards-climate-catastrophe-nagraj-adve-21393', 'meta_title' => null, 'meta_keywords' => null, 'meta_description' => null, 'noindex' => (int) 0, 'publish_date' => object(Cake\I18n\FrozenDate) {}, 'most_visit_section_id' => null, 'article_big_img' => null, 'liveid' => (int) 21393, 'created' => object(Cake\I18n\FrozenTime) {}, 'modified' => object(Cake\I18n\FrozenTime) {}, 'edate' => '', 'tags' => [ [maximum depth reached] ], 'category' => object(App\Model\Entity\Category) {}, '[new]' => false, '[accessible]' => [ [maximum depth reached] ], '[dirty]' => [[maximum depth reached]], '[original]' => [[maximum depth reached]], '[virtual]' => [[maximum depth reached]], '[hasErrors]' => false, '[errors]' => [[maximum depth reached]], '[invalid]' => [[maximum depth reached]], '[repository]' => 'Articles' }, 'articleid' => (int) 21248, 'metaTitle' => 'LATEST NEWS UPDATES | A race towards climate catastrophe-Nagraj Adve', 'metaKeywords' => 'Global Warming,climate change,Environment', 'metaDesc' => ' -The Hindu &nbsp; &nbsp; The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it...', 'disp' => '<div align="justify">-The Hindu</div><p align="justify">&nbsp;</p><p align="justify">&nbsp;</p><p align="justify"><em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em></p><p align="justify">When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons.</p><p align="justify"><em>Impact on life cycles</em></p><p align="justify">One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade.</p><p align="justify">This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species.</p><p align="justify">This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or &quot;been the first groups in which whole species have gone extinct due to recent climate change.&quot;</p><p align="justify">Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that &quot;if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that&quot; (&quot;Target Atmospheric CO: Where Should Humanity Aim?,&quot; The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org.</p><p align="justify"><em>Temperature regulator</em></p><p align="justify">Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: &quot;The similarity between CO and temperature in [the] Antarctica is jaw-dropping,&quot; a causal link he says that's even stronger than that between smoking and lung cancer, &quot;kind of a gold standard in the medical world.&quot; Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience.</p><p align="justify">We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop.</p><p align="justify"><em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em></p>', 'lang' => 'English', 'SITE_URL' => 'https://im4change.in/', 'site_title' => 'im4change', 'adminprix' => 'admin' ] $article_current = object(App\Model\Entity\Article) { 'id' => (int) 21248, 'title' => 'A race towards climate catastrophe-Nagraj Adve', 'subheading' => '', 'description' => '<div align="justify"> -The Hindu </div> <p align="justify"> &nbsp; </p> <p align="justify"> &nbsp; </p> <p align="justify"> <em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em> </p> <p align="justify"> When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons. </p> <p align="justify"> <em>Impact on life cycles</em> </p> <p align="justify"> One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade. </p> <p align="justify"> This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species. </p> <p align="justify"> This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or &quot;been the first groups in which whole species have gone extinct due to recent climate change.&quot; </p> <p align="justify"> Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that &quot;if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that&quot; (&quot;Target Atmospheric CO: Where Should Humanity Aim?,&quot; The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org. </p> <p align="justify"> <em>Temperature regulator</em> </p> <p align="justify"> Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: &quot;The similarity between CO and temperature in [the] Antarctica is jaw-dropping,&quot; a causal link he says that's even stronger than that between smoking and lung cancer, &quot;kind of a gold standard in the medical world.&quot; Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience. </p> <p align="justify"> We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop. </p> <p align="justify"> <em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em> </p>', 'credit_writer' => 'The Hindu, 4 June, 2013, http://www.thehindu.com/opinion/op-ed/a-race-towards-climate-catastrophe/article4778996.ece', 'article_img' => '', 'article_img_thumb' => '', 'status' => (int) 1, 'show_on_home' => (int) 1, 'lang' => 'EN', 'category_id' => (int) 16, 'tag_keyword' => '', 'seo_url' => 'a-race-towards-climate-catastrophe-nagraj-adve-21393', 'meta_title' => null, 'meta_keywords' => null, 'meta_description' => null, 'noindex' => (int) 0, 'publish_date' => object(Cake\I18n\FrozenDate) {}, 'most_visit_section_id' => null, 'article_big_img' => null, 'liveid' => (int) 21393, 'created' => object(Cake\I18n\FrozenTime) {}, 'modified' => object(Cake\I18n\FrozenTime) {}, 'edate' => '', 'tags' => [ (int) 0 => object(Cake\ORM\Entity) {}, (int) 1 => object(Cake\ORM\Entity) {}, (int) 2 => object(Cake\ORM\Entity) {} ], 'category' => object(App\Model\Entity\Category) {}, '[new]' => false, '[accessible]' => [ '*' => true, 'id' => false ], '[dirty]' => [], '[original]' => [], '[virtual]' => [], '[hasErrors]' => false, '[errors]' => [], '[invalid]' => [], '[repository]' => 'Articles' } $articleid = (int) 21248 $metaTitle = 'LATEST NEWS UPDATES | A race towards climate catastrophe-Nagraj Adve' $metaKeywords = 'Global Warming,climate change,Environment' $metaDesc = ' -The Hindu &nbsp; &nbsp; The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it...' $disp = '<div align="justify">-The Hindu</div><p align="justify">&nbsp;</p><p align="justify">&nbsp;</p><p align="justify"><em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em></p><p align="justify">When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons.</p><p align="justify"><em>Impact on life cycles</em></p><p align="justify">One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade.</p><p align="justify">This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species.</p><p align="justify">This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or &quot;been the first groups in which whole species have gone extinct due to recent climate change.&quot;</p><p align="justify">Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that &quot;if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that&quot; (&quot;Target Atmospheric CO: Where Should Humanity Aim?,&quot; The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org.</p><p align="justify"><em>Temperature regulator</em></p><p align="justify">Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: &quot;The similarity between CO and temperature in [the] Antarctica is jaw-dropping,&quot; a causal link he says that's even stronger than that between smoking and lung cancer, &quot;kind of a gold standard in the medical world.&quot; Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience.</p><p align="justify">We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop.</p><p align="justify"><em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em></p>' $lang = 'English' $SITE_URL = 'https://im4change.in/' $site_title = 'im4change' $adminprix = 'admin'</pre><pre class="stack-trace">include - APP/Template/Layout/printlayout.ctp, line 8 Cake\View\View::_evaluate() - CORE/src/View/View.php, line 1413 Cake\View\View::_render() - CORE/src/View/View.php, line 1374 Cake\View\View::renderLayout() - CORE/src/View/View.php, line 927 Cake\View\View::render() - CORE/src/View/View.php, line 885 Cake\Controller\Controller::render() - CORE/src/Controller/Controller.php, line 791 Cake\Http\ActionDispatcher::_invoke() - CORE/src/Http/ActionDispatcher.php, line 126 Cake\Http\ActionDispatcher::dispatch() - CORE/src/Http/ActionDispatcher.php, line 94 Cake\Http\BaseApplication::__invoke() - CORE/src/Http/BaseApplication.php, line 235 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Routing\Middleware\RoutingMiddleware::__invoke() - CORE/src/Routing/Middleware/RoutingMiddleware.php, line 162 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Routing\Middleware\AssetMiddleware::__invoke() - CORE/src/Routing/Middleware/AssetMiddleware.php, line 88 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Error\Middleware\ErrorHandlerMiddleware::__invoke() - CORE/src/Error/Middleware/ErrorHandlerMiddleware.php, line 96 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Http\Runner::run() - CORE/src/Http/Runner.php, line 51</pre></div></pre>latest-news-updates/a-race-towards-climate-catastrophe-nagraj-adve-21393.html"/> <meta http-equiv="Content-Type" content="text/html; charset=utf-8"/> <link href="https://im4change.in/css/control.css" rel="stylesheet" type="text/css" media="all"/> <title>LATEST NEWS UPDATES | A race towards climate catastrophe-Nagraj Adve | Im4change.org</title> <meta name="description" content=" -The Hindu The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it..."/> <script src="https://im4change.in/js/jquery-1.10.2.js"></script> <script type="text/javascript" src="https://im4change.in/js/jquery-migrate.min.js"></script> <script language="javascript" type="text/javascript"> $(document).ready(function () { var img = $("img")[0]; // Get my img elem var pic_real_width, pic_real_height; $("<img/>") // Make in memory copy of image to avoid css issues .attr("src", $(img).attr("src")) .load(function () { pic_real_width = this.width; // Note: $(this).width() will not pic_real_height = this.height; // work for in memory images. }); }); </script> <style type="text/css"> @media screen { div.divFooter { display: block; } } @media print { .printbutton { display: none !important; } } </style> </head> <body> <table cellpadding="0" cellspacing="0" border="0" width="98%" align="center"> <tr> <td class="top_bg"> <div class="divFooter"> <img src="https://im4change.in/images/logo1.jpg" height="59" border="0" alt="Resource centre on India's rural distress" style="padding-top:14px;"/> </div> </td> </tr> <tr> <td id="topspace"> </td> </tr> <tr id="topspace"> <td> </td> </tr> <tr> <td height="50" style="border-bottom:1px solid #000; padding-top:10px;" class="printbutton"> <form><input type="button" value=" Print this page " onclick="window.print();return false;"/></form> </td> </tr> <tr> <td width="100%"> <h1 class="news_headlines" style="font-style:normal"> <strong>A race towards climate catastrophe-Nagraj Adve</strong></h1> </td> </tr> <tr> <td width="100%" style="font-family:Arial, 'Segoe Script', 'Segoe UI', sans-serif, serif"><font size="3"> <div align="justify">-The Hindu</div><p align="justify"> </p><p align="justify"> </p><p align="justify"><em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em></p><p align="justify">When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons.</p><p align="justify"><em>Impact on life cycles</em></p><p align="justify">One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade.</p><p align="justify">This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species.</p><p align="justify">This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or "been the first groups in which whole species have gone extinct due to recent climate change."</p><p align="justify">Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that "if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that" ("Target Atmospheric CO: Where Should Humanity Aim?," The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org.</p><p align="justify"><em>Temperature regulator</em></p><p align="justify">Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: "The similarity between CO and temperature in [the] Antarctica is jaw-dropping," a causal link he says that's even stronger than that between smoking and lung cancer, "kind of a gold standard in the medical world." Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience.</p><p align="justify">We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop.</p><p align="justify"><em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em></p> </font> </td> </tr> <tr> <td> </td> </tr> <tr> <td height="50" style="border-top:1px solid #000; border-bottom:1px solid #000;padding-top:10px;"> <form><input type="button" value=" Print this page " onclick="window.print();return false;"/></form> </td> </tr> </table></body> </html>' } $maxBufferLength = (int) 8192 $file = '/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Error/Debugger.php' $line = (int) 853 $message = 'Unable to emit headers. Headers sent in file=/home/brlfuser/public_html/vendor/cakephp/cakephp/src/Error/Debugger.php line=853'Cake\Http\ResponseEmitter::emit() - CORE/src/Http/ResponseEmitter.php, line 48 Cake\Http\Server::emit() - CORE/src/Http/Server.php, line 141 [main] - ROOT/webroot/index.php, line 39
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'' : 'none');"><b>Notice</b> (8)</a>: Undefined variable: urlPrefix [<b>APP/Template/Layout/printlayout.ctp</b>, line <b>8</b>]<div id="cakeErr68035bdbe069d-trace" class="cake-stack-trace" style="display: none;"><a href="javascript:void(0);" onclick="document.getElementById('cakeErr68035bdbe069d-code').style.display = (document.getElementById('cakeErr68035bdbe069d-code').style.display == 'none' ? '' : 'none')">Code</a> <a href="javascript:void(0);" onclick="document.getElementById('cakeErr68035bdbe069d-context').style.display = (document.getElementById('cakeErr68035bdbe069d-context').style.display == 'none' ? '' : 'none')">Context</a><pre id="cakeErr68035bdbe069d-code" class="cake-code-dump" style="display: none;"><code><span style="color: #000000"><span style="color: #0000BB"></span><span style="color: #007700"><</span><span style="color: #0000BB">head</span><span style="color: #007700">> </span></span></code> <span class="code-highlight"><code><span style="color: #000000"> <link rel="canonical" href="<span style="color: #0000BB"><?php </span><span style="color: #007700">echo </span><span style="color: #0000BB">Configure</span><span style="color: #007700">::</span><span style="color: #0000BB">read</span><span style="color: #007700">(</span><span style="color: #DD0000">'SITE_URL'</span><span style="color: #007700">); </span><span style="color: #0000BB">?><?php </span><span style="color: #007700">echo </span><span style="color: #0000BB">$urlPrefix</span><span style="color: #007700">;</span><span style="color: #0000BB">?><?php </span><span style="color: #007700">echo </span><span style="color: #0000BB">$article_current</span><span style="color: #007700">-></span><span style="color: #0000BB">category</span><span style="color: #007700">-></span><span style="color: #0000BB">slug</span><span style="color: #007700">; </span><span style="color: #0000BB">?></span>/<span style="color: #0000BB"><?php </span><span style="color: #007700">echo </span><span style="color: #0000BB">$article_current</span><span style="color: #007700">-></span><span style="color: #0000BB">seo_url</span><span style="color: #007700">; </span><span style="color: #0000BB">?></span>.html"/> </span></code></span> <code><span style="color: #000000"><span style="color: #0000BB"> </span><span style="color: #007700"><</span><span style="color: #0000BB">meta http</span><span style="color: #007700">-</span><span style="color: #0000BB">equiv</span><span style="color: #007700">=</span><span style="color: #DD0000">"Content-Type" </span><span style="color: #0000BB">content</span><span style="color: #007700">=</span><span style="color: #DD0000">"text/html; charset=utf-8"</span><span style="color: #007700">/> </span></span></code></pre><pre id="cakeErr68035bdbe069d-context" class="cake-context" style="display: none;">$viewFile = '/home/brlfuser/public_html/src/Template/Layout/printlayout.ctp' $dataForView = [ 'article_current' => object(App\Model\Entity\Article) { 'id' => (int) 21248, 'title' => 'A race towards climate catastrophe-Nagraj Adve', 'subheading' => '', 'description' => '<div align="justify"> -The Hindu </div> <p align="justify"> &nbsp; </p> <p align="justify"> &nbsp; </p> <p align="justify"> <em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em> </p> <p align="justify"> When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons. </p> <p align="justify"> <em>Impact on life cycles</em> </p> <p align="justify"> One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade. </p> <p align="justify"> This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species. </p> <p align="justify"> This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or &quot;been the first groups in which whole species have gone extinct due to recent climate change.&quot; </p> <p align="justify"> Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that &quot;if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that&quot; (&quot;Target Atmospheric CO: Where Should Humanity Aim?,&quot; The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org. </p> <p align="justify"> <em>Temperature regulator</em> </p> <p align="justify"> Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: &quot;The similarity between CO and temperature in [the] Antarctica is jaw-dropping,&quot; a causal link he says that's even stronger than that between smoking and lung cancer, &quot;kind of a gold standard in the medical world.&quot; Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience. </p> <p align="justify"> We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop. </p> <p align="justify"> <em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em> </p>', 'credit_writer' => 'The Hindu, 4 June, 2013, http://www.thehindu.com/opinion/op-ed/a-race-towards-climate-catastrophe/article4778996.ece', 'article_img' => '', 'article_img_thumb' => '', 'status' => (int) 1, 'show_on_home' => (int) 1, 'lang' => 'EN', 'category_id' => (int) 16, 'tag_keyword' => '', 'seo_url' => 'a-race-towards-climate-catastrophe-nagraj-adve-21393', 'meta_title' => null, 'meta_keywords' => null, 'meta_description' => null, 'noindex' => (int) 0, 'publish_date' => object(Cake\I18n\FrozenDate) {}, 'most_visit_section_id' => null, 'article_big_img' => null, 'liveid' => (int) 21393, 'created' => object(Cake\I18n\FrozenTime) {}, 'modified' => object(Cake\I18n\FrozenTime) {}, 'edate' => '', 'tags' => [ [maximum depth reached] ], 'category' => object(App\Model\Entity\Category) {}, '[new]' => false, '[accessible]' => [ [maximum depth reached] ], '[dirty]' => [[maximum depth reached]], '[original]' => [[maximum depth reached]], '[virtual]' => [[maximum depth reached]], '[hasErrors]' => false, '[errors]' => [[maximum depth reached]], '[invalid]' => [[maximum depth reached]], '[repository]' => 'Articles' }, 'articleid' => (int) 21248, 'metaTitle' => 'LATEST NEWS UPDATES | A race towards climate catastrophe-Nagraj Adve', 'metaKeywords' => 'Global Warming,climate change,Environment', 'metaDesc' => ' -The Hindu &nbsp; &nbsp; The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it...', 'disp' => '<div align="justify">-The Hindu</div><p align="justify">&nbsp;</p><p align="justify">&nbsp;</p><p align="justify"><em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em></p><p align="justify">When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons.</p><p align="justify"><em>Impact on life cycles</em></p><p align="justify">One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade.</p><p align="justify">This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species.</p><p align="justify">This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or &quot;been the first groups in which whole species have gone extinct due to recent climate change.&quot;</p><p align="justify">Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that &quot;if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that&quot; (&quot;Target Atmospheric CO: Where Should Humanity Aim?,&quot; The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org.</p><p align="justify"><em>Temperature regulator</em></p><p align="justify">Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: &quot;The similarity between CO and temperature in [the] Antarctica is jaw-dropping,&quot; a causal link he says that's even stronger than that between smoking and lung cancer, &quot;kind of a gold standard in the medical world.&quot; Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience.</p><p align="justify">We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop.</p><p align="justify"><em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em></p>', 'lang' => 'English', 'SITE_URL' => 'https://im4change.in/', 'site_title' => 'im4change', 'adminprix' => 'admin' ] $article_current = object(App\Model\Entity\Article) { 'id' => (int) 21248, 'title' => 'A race towards climate catastrophe-Nagraj Adve', 'subheading' => '', 'description' => '<div align="justify"> -The Hindu </div> <p align="justify"> &nbsp; </p> <p align="justify"> &nbsp; </p> <p align="justify"> <em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em> </p> <p align="justify"> When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons. </p> <p align="justify"> <em>Impact on life cycles</em> </p> <p align="justify"> One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade. </p> <p align="justify"> This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species. </p> <p align="justify"> This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or &quot;been the first groups in which whole species have gone extinct due to recent climate change.&quot; </p> <p align="justify"> Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that &quot;if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that&quot; (&quot;Target Atmospheric CO: Where Should Humanity Aim?,&quot; The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org. </p> <p align="justify"> <em>Temperature regulator</em> </p> <p align="justify"> Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: &quot;The similarity between CO and temperature in [the] Antarctica is jaw-dropping,&quot; a causal link he says that's even stronger than that between smoking and lung cancer, &quot;kind of a gold standard in the medical world.&quot; Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience. </p> <p align="justify"> We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop. </p> <p align="justify"> <em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em> </p>', 'credit_writer' => 'The Hindu, 4 June, 2013, http://www.thehindu.com/opinion/op-ed/a-race-towards-climate-catastrophe/article4778996.ece', 'article_img' => '', 'article_img_thumb' => '', 'status' => (int) 1, 'show_on_home' => (int) 1, 'lang' => 'EN', 'category_id' => (int) 16, 'tag_keyword' => '', 'seo_url' => 'a-race-towards-climate-catastrophe-nagraj-adve-21393', 'meta_title' => null, 'meta_keywords' => null, 'meta_description' => null, 'noindex' => (int) 0, 'publish_date' => object(Cake\I18n\FrozenDate) {}, 'most_visit_section_id' => null, 'article_big_img' => null, 'liveid' => (int) 21393, 'created' => object(Cake\I18n\FrozenTime) {}, 'modified' => object(Cake\I18n\FrozenTime) {}, 'edate' => '', 'tags' => [ (int) 0 => object(Cake\ORM\Entity) {}, (int) 1 => object(Cake\ORM\Entity) {}, (int) 2 => object(Cake\ORM\Entity) {} ], 'category' => object(App\Model\Entity\Category) {}, '[new]' => false, '[accessible]' => [ '*' => true, 'id' => false ], '[dirty]' => [], '[original]' => [], '[virtual]' => [], '[hasErrors]' => false, '[errors]' => [], '[invalid]' => [], '[repository]' => 'Articles' } $articleid = (int) 21248 $metaTitle = 'LATEST NEWS UPDATES | A race towards climate catastrophe-Nagraj Adve' $metaKeywords = 'Global Warming,climate change,Environment' $metaDesc = ' -The Hindu &nbsp; &nbsp; The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it...' $disp = '<div align="justify">-The Hindu</div><p align="justify">&nbsp;</p><p align="justify">&nbsp;</p><p align="justify"><em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em></p><p align="justify">When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons.</p><p align="justify"><em>Impact on life cycles</em></p><p align="justify">One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade.</p><p align="justify">This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species.</p><p align="justify">This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or &quot;been the first groups in which whole species have gone extinct due to recent climate change.&quot;</p><p align="justify">Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that &quot;if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that&quot; (&quot;Target Atmospheric CO: Where Should Humanity Aim?,&quot; The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org.</p><p align="justify"><em>Temperature regulator</em></p><p align="justify">Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: &quot;The similarity between CO and temperature in [the] Antarctica is jaw-dropping,&quot; a causal link he says that's even stronger than that between smoking and lung cancer, &quot;kind of a gold standard in the medical world.&quot; Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience.</p><p align="justify">We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop.</p><p align="justify"><em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em></p>' $lang = 'English' $SITE_URL = 'https://im4change.in/' $site_title = 'im4change' $adminprix = 'admin'</pre><pre class="stack-trace">include - APP/Template/Layout/printlayout.ctp, line 8 Cake\View\View::_evaluate() - CORE/src/View/View.php, line 1413 Cake\View\View::_render() - CORE/src/View/View.php, line 1374 Cake\View\View::renderLayout() - CORE/src/View/View.php, line 927 Cake\View\View::render() - CORE/src/View/View.php, line 885 Cake\Controller\Controller::render() - CORE/src/Controller/Controller.php, line 791 Cake\Http\ActionDispatcher::_invoke() - CORE/src/Http/ActionDispatcher.php, line 126 Cake\Http\ActionDispatcher::dispatch() - CORE/src/Http/ActionDispatcher.php, line 94 Cake\Http\BaseApplication::__invoke() - CORE/src/Http/BaseApplication.php, line 235 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Routing\Middleware\RoutingMiddleware::__invoke() - CORE/src/Routing/Middleware/RoutingMiddleware.php, line 162 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Routing\Middleware\AssetMiddleware::__invoke() - CORE/src/Routing/Middleware/AssetMiddleware.php, line 88 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Error\Middleware\ErrorHandlerMiddleware::__invoke() - CORE/src/Error/Middleware/ErrorHandlerMiddleware.php, line 96 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Http\Runner::run() - CORE/src/Http/Runner.php, line 51</pre></div></pre>latest-news-updates/a-race-towards-climate-catastrophe-nagraj-adve-21393.html"/> <meta http-equiv="Content-Type" content="text/html; charset=utf-8"/> <link href="https://im4change.in/css/control.css" rel="stylesheet" type="text/css" media="all"/> <title>LATEST NEWS UPDATES | A race towards climate catastrophe-Nagraj Adve | Im4change.org</title> <meta name="description" content=" -The Hindu The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it..."/> <script src="https://im4change.in/js/jquery-1.10.2.js"></script> <script type="text/javascript" src="https://im4change.in/js/jquery-migrate.min.js"></script> <script language="javascript" type="text/javascript"> $(document).ready(function () { var img = $("img")[0]; // Get my img elem var pic_real_width, pic_real_height; $("<img/>") // Make in memory copy of image to avoid css issues .attr("src", $(img).attr("src")) .load(function () { pic_real_width = this.width; // Note: $(this).width() will not pic_real_height = this.height; // work for in memory images. }); }); </script> <style type="text/css"> @media screen { div.divFooter { display: block; } } @media print { .printbutton { display: none !important; } } </style> </head> <body> <table cellpadding="0" cellspacing="0" border="0" width="98%" align="center"> <tr> <td class="top_bg"> <div class="divFooter"> <img src="https://im4change.in/images/logo1.jpg" height="59" border="0" alt="Resource centre on India's rural distress" style="padding-top:14px;"/> </div> </td> </tr> <tr> <td id="topspace"> </td> </tr> <tr id="topspace"> <td> </td> </tr> <tr> <td height="50" style="border-bottom:1px solid #000; padding-top:10px;" class="printbutton"> <form><input type="button" value=" Print this page " onclick="window.print();return false;"/></form> </td> </tr> <tr> <td width="100%"> <h1 class="news_headlines" style="font-style:normal"> <strong>A race towards climate catastrophe-Nagraj Adve</strong></h1> </td> </tr> <tr> <td width="100%" style="font-family:Arial, 'Segoe Script', 'Segoe UI', sans-serif, serif"><font size="3"> <div align="justify">-The Hindu</div><p align="justify"> </p><p align="justify"> </p><p align="justify"><em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em></p><p align="justify">When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons.</p><p align="justify"><em>Impact on life cycles</em></p><p align="justify">One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade.</p><p align="justify">This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species.</p><p align="justify">This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or "been the first groups in which whole species have gone extinct due to recent climate change."</p><p align="justify">Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that "if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that" ("Target Atmospheric CO: Where Should Humanity Aim?," The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org.</p><p align="justify"><em>Temperature regulator</em></p><p align="justify">Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: "The similarity between CO and temperature in [the] Antarctica is jaw-dropping," a causal link he says that's even stronger than that between smoking and lung cancer, "kind of a gold standard in the medical world." Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience.</p><p align="justify">We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop.</p><p align="justify"><em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em></p> </font> </td> </tr> <tr> <td> </td> </tr> <tr> <td height="50" style="border-top:1px solid #000; border-bottom:1px solid #000;padding-top:10px;"> <form><input type="button" value=" Print this page " onclick="window.print();return false;"/></form> </td> </tr> </table></body> </html>' } $reasonPhrase = 'OK'header - [internal], line ?? 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'' : 'none');"><b>Notice</b> (8)</a>: Undefined variable: urlPrefix [<b>APP/Template/Layout/printlayout.ctp</b>, line <b>8</b>]<div id="cakeErr68035bdbe069d-trace" class="cake-stack-trace" style="display: none;"><a href="javascript:void(0);" onclick="document.getElementById('cakeErr68035bdbe069d-code').style.display = (document.getElementById('cakeErr68035bdbe069d-code').style.display == 'none' ? '' : 'none')">Code</a> <a href="javascript:void(0);" onclick="document.getElementById('cakeErr68035bdbe069d-context').style.display = (document.getElementById('cakeErr68035bdbe069d-context').style.display == 'none' ? '' : 'none')">Context</a><pre id="cakeErr68035bdbe069d-code" class="cake-code-dump" style="display: none;"><code><span style="color: #000000"><span style="color: #0000BB"></span><span style="color: #007700"><</span><span style="color: #0000BB">head</span><span style="color: #007700">> </span></span></code> <span class="code-highlight"><code><span style="color: #000000"> <link rel="canonical" href="<span style="color: #0000BB"><?php </span><span style="color: #007700">echo </span><span style="color: #0000BB">Configure</span><span style="color: #007700">::</span><span style="color: #0000BB">read</span><span style="color: #007700">(</span><span style="color: #DD0000">'SITE_URL'</span><span style="color: #007700">); </span><span style="color: #0000BB">?><?php </span><span style="color: #007700">echo </span><span style="color: #0000BB">$urlPrefix</span><span style="color: #007700">;</span><span style="color: #0000BB">?><?php </span><span style="color: #007700">echo </span><span style="color: #0000BB">$article_current</span><span style="color: #007700">-></span><span style="color: #0000BB">category</span><span style="color: #007700">-></span><span style="color: #0000BB">slug</span><span style="color: #007700">; </span><span style="color: #0000BB">?></span>/<span style="color: #0000BB"><?php </span><span style="color: #007700">echo </span><span style="color: #0000BB">$article_current</span><span style="color: #007700">-></span><span style="color: #0000BB">seo_url</span><span style="color: #007700">; </span><span style="color: #0000BB">?></span>.html"/> </span></code></span> <code><span style="color: #000000"><span style="color: #0000BB"> </span><span style="color: #007700"><</span><span style="color: #0000BB">meta http</span><span style="color: #007700">-</span><span style="color: #0000BB">equiv</span><span style="color: #007700">=</span><span style="color: #DD0000">"Content-Type" </span><span style="color: #0000BB">content</span><span style="color: #007700">=</span><span style="color: #DD0000">"text/html; charset=utf-8"</span><span style="color: #007700">/> </span></span></code></pre><pre id="cakeErr68035bdbe069d-context" class="cake-context" style="display: none;">$viewFile = '/home/brlfuser/public_html/src/Template/Layout/printlayout.ctp' $dataForView = [ 'article_current' => object(App\Model\Entity\Article) { 'id' => (int) 21248, 'title' => 'A race towards climate catastrophe-Nagraj Adve', 'subheading' => '', 'description' => '<div align="justify"> -The Hindu </div> <p align="justify"> &nbsp; </p> <p align="justify"> &nbsp; </p> <p align="justify"> <em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em> </p> <p align="justify"> When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons. </p> <p align="justify"> <em>Impact on life cycles</em> </p> <p align="justify"> One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade. </p> <p align="justify"> This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species. </p> <p align="justify"> This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or &quot;been the first groups in which whole species have gone extinct due to recent climate change.&quot; </p> <p align="justify"> Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that &quot;if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that&quot; (&quot;Target Atmospheric CO: Where Should Humanity Aim?,&quot; The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org. </p> <p align="justify"> <em>Temperature regulator</em> </p> <p align="justify"> Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: &quot;The similarity between CO and temperature in [the] Antarctica is jaw-dropping,&quot; a causal link he says that's even stronger than that between smoking and lung cancer, &quot;kind of a gold standard in the medical world.&quot; Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience. </p> <p align="justify"> We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. 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There is no more room for manoeuvre When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it...', 'disp' => '<div align="justify">-The Hindu</div><p align="justify">&nbsp;</p><p align="justify">&nbsp;</p><p align="justify"><em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em></p><p align="justify">When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons.</p><p align="justify"><em>Impact on life cycles</em></p><p align="justify">One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade.</p><p align="justify">This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species.</p><p align="justify">This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or &quot;been the first groups in which whole species have gone extinct due to recent climate change.&quot;</p><p align="justify">Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that &quot;if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that&quot; (&quot;Target Atmospheric CO: Where Should Humanity Aim?,&quot; The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org.</p><p align="justify"><em>Temperature regulator</em></p><p align="justify">Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: &quot;The similarity between CO and temperature in [the] Antarctica is jaw-dropping,&quot; a causal link he says that's even stronger than that between smoking and lung cancer, &quot;kind of a gold standard in the medical world.&quot; Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience.</p><p align="justify">We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop.</p><p align="justify"><em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em></p>', 'lang' => 'English', 'SITE_URL' => 'https://im4change.in/', 'site_title' => 'im4change', 'adminprix' => 'admin' ] $article_current = object(App\Model\Entity\Article) { 'id' => (int) 21248, 'title' => 'A race towards climate catastrophe-Nagraj Adve', 'subheading' => '', 'description' => '<div align="justify"> -The Hindu </div> <p align="justify"> &nbsp; </p> <p align="justify"> &nbsp; </p> <p align="justify"> <em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em> </p> <p align="justify"> When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons. </p> <p align="justify"> <em>Impact on life cycles</em> </p> <p align="justify"> One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade. </p> <p align="justify"> This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species. </p> <p align="justify"> This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or &quot;been the first groups in which whole species have gone extinct due to recent climate change.&quot; </p> <p align="justify"> Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that &quot;if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that&quot; (&quot;Target Atmospheric CO: Where Should Humanity Aim?,&quot; The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org. </p> <p align="justify"> <em>Temperature regulator</em> </p> <p align="justify"> Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: &quot;The similarity between CO and temperature in [the] Antarctica is jaw-dropping,&quot; a causal link he says that's even stronger than that between smoking and lung cancer, &quot;kind of a gold standard in the medical world.&quot; Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience. </p> <p align="justify"> We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop. </p> <p align="justify"> <em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em> </p>', 'credit_writer' => 'The Hindu, 4 June, 2013, http://www.thehindu.com/opinion/op-ed/a-race-towards-climate-catastrophe/article4778996.ece', 'article_img' => '', 'article_img_thumb' => '', 'status' => (int) 1, 'show_on_home' => (int) 1, 'lang' => 'EN', 'category_id' => (int) 16, 'tag_keyword' => '', 'seo_url' => 'a-race-towards-climate-catastrophe-nagraj-adve-21393', 'meta_title' => null, 'meta_keywords' => null, 'meta_description' => null, 'noindex' => (int) 0, 'publish_date' => object(Cake\I18n\FrozenDate) {}, 'most_visit_section_id' => null, 'article_big_img' => null, 'liveid' => (int) 21393, 'created' => object(Cake\I18n\FrozenTime) {}, 'modified' => object(Cake\I18n\FrozenTime) {}, 'edate' => '', 'tags' => [ (int) 0 => object(Cake\ORM\Entity) {}, (int) 1 => object(Cake\ORM\Entity) {}, (int) 2 => object(Cake\ORM\Entity) {} ], 'category' => object(App\Model\Entity\Category) {}, '[new]' => false, '[accessible]' => [ '*' => true, 'id' => false ], '[dirty]' => [], '[original]' => [], '[virtual]' => [], '[hasErrors]' => false, '[errors]' => [], '[invalid]' => [], '[repository]' => 'Articles' } $articleid = (int) 21248 $metaTitle = 'LATEST NEWS UPDATES | A race towards climate catastrophe-Nagraj Adve' $metaKeywords = 'Global Warming,climate change,Environment' $metaDesc = ' -The Hindu &nbsp; &nbsp; The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it...' $disp = '<div align="justify">-The Hindu</div><p align="justify">&nbsp;</p><p align="justify">&nbsp;</p><p align="justify"><em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em></p><p align="justify">When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons.</p><p align="justify"><em>Impact on life cycles</em></p><p align="justify">One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade.</p><p align="justify">This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species.</p><p align="justify">This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or &quot;been the first groups in which whole species have gone extinct due to recent climate change.&quot;</p><p align="justify">Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that &quot;if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that&quot; (&quot;Target Atmospheric CO: Where Should Humanity Aim?,&quot; The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org.</p><p align="justify"><em>Temperature regulator</em></p><p align="justify">Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: &quot;The similarity between CO and temperature in [the] Antarctica is jaw-dropping,&quot; a causal link he says that's even stronger than that between smoking and lung cancer, &quot;kind of a gold standard in the medical world.&quot; Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience.</p><p align="justify">We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop.</p><p align="justify"><em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em></p>' $lang = 'English' $SITE_URL = 'https://im4change.in/' $site_title = 'im4change' $adminprix = 'admin'</pre><pre class="stack-trace">include - APP/Template/Layout/printlayout.ctp, line 8 Cake\View\View::_evaluate() - CORE/src/View/View.php, line 1413 Cake\View\View::_render() - CORE/src/View/View.php, line 1374 Cake\View\View::renderLayout() - CORE/src/View/View.php, line 927 Cake\View\View::render() - CORE/src/View/View.php, line 885 Cake\Controller\Controller::render() - CORE/src/Controller/Controller.php, line 791 Cake\Http\ActionDispatcher::_invoke() - CORE/src/Http/ActionDispatcher.php, line 126 Cake\Http\ActionDispatcher::dispatch() - CORE/src/Http/ActionDispatcher.php, line 94 Cake\Http\BaseApplication::__invoke() - CORE/src/Http/BaseApplication.php, line 235 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Routing\Middleware\RoutingMiddleware::__invoke() - CORE/src/Routing/Middleware/RoutingMiddleware.php, line 162 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Routing\Middleware\AssetMiddleware::__invoke() - CORE/src/Routing/Middleware/AssetMiddleware.php, line 88 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Error\Middleware\ErrorHandlerMiddleware::__invoke() - CORE/src/Error/Middleware/ErrorHandlerMiddleware.php, line 96 Cake\Http\Runner::__invoke() - CORE/src/Http/Runner.php, line 65 Cake\Http\Runner::run() - CORE/src/Http/Runner.php, line 51</pre></div></pre>latest-news-updates/a-race-towards-climate-catastrophe-nagraj-adve-21393.html"/> <meta http-equiv="Content-Type" content="text/html; charset=utf-8"/> <link href="https://im4change.in/css/control.css" rel="stylesheet" type="text/css" media="all"/> <title>LATEST NEWS UPDATES | A race towards climate catastrophe-Nagraj Adve | Im4change.org</title> <meta name="description" content=" -The Hindu The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it..."/> <script src="https://im4change.in/js/jquery-1.10.2.js"></script> <script type="text/javascript" src="https://im4change.in/js/jquery-migrate.min.js"></script> <script language="javascript" type="text/javascript"> $(document).ready(function () { var img = $("img")[0]; // Get my img elem var pic_real_width, pic_real_height; $("<img/>") // Make in memory copy of image to avoid css issues .attr("src", $(img).attr("src")) .load(function () { pic_real_width = this.width; // Note: $(this).width() will not pic_real_height = this.height; // work for in memory images. }); }); </script> <style type="text/css"> @media screen { div.divFooter { display: block; } } @media print { .printbutton { display: none !important; } } </style> </head> <body> <table cellpadding="0" cellspacing="0" border="0" width="98%" align="center"> <tr> <td class="top_bg"> <div class="divFooter"> <img src="https://im4change.in/images/logo1.jpg" height="59" border="0" alt="Resource centre on India's rural distress" style="padding-top:14px;"/> </div> </td> </tr> <tr> <td id="topspace"> </td> </tr> <tr id="topspace"> <td> </td> </tr> <tr> <td height="50" style="border-bottom:1px solid #000; padding-top:10px;" class="printbutton"> <form><input type="button" value=" Print this page " onclick="window.print();return false;"/></form> </td> </tr> <tr> <td width="100%"> <h1 class="news_headlines" style="font-style:normal"> <strong>A race towards climate catastrophe-Nagraj Adve</strong></h1> </td> </tr> <tr> <td width="100%" style="font-family:Arial, 'Segoe Script', 'Segoe UI', sans-serif, serif"><font size="3"> <div align="justify">-The Hindu</div><p align="justify"> </p><p align="justify"> </p><p align="justify"><em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em></p><p align="justify">When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons.</p><p align="justify"><em>Impact on life cycles</em></p><p align="justify">One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade.</p><p align="justify">This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species.</p><p align="justify">This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or "been the first groups in which whole species have gone extinct due to recent climate change."</p><p align="justify">Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that "if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that" ("Target Atmospheric CO: Where Should Humanity Aim?," The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org.</p><p align="justify"><em>Temperature regulator</em></p><p align="justify">Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: "The similarity between CO and temperature in [the] Antarctica is jaw-dropping," a causal link he says that's even stronger than that between smoking and lung cancer, "kind of a gold standard in the medical world." Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience.</p><p align="justify">We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop.</p><p align="justify"><em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em></p> </font> </td> </tr> <tr> <td> </td> </tr> <tr> <td height="50" style="border-top:1px solid #000; border-bottom:1px solid #000;padding-top:10px;"> <form><input type="button" value=" Print this page " onclick="window.print();return false;"/></form> </td> </tr> </table></body> </html>' } $cookies = [] $values = [ (int) 0 => 'text/html; charset=UTF-8' ] $name = 'Content-Type' $first = true $value = 'text/html; charset=UTF-8'header - [internal], line ?? Cake\Http\ResponseEmitter::emitHeaders() - CORE/src/Http/ResponseEmitter.php, line 181 Cake\Http\ResponseEmitter::emit() - CORE/src/Http/ResponseEmitter.php, line 55 Cake\Http\Server::emit() - CORE/src/Http/Server.php, line 141 [main] - ROOT/webroot/index.php, line 39
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$viewFile = '/home/brlfuser/public_html/src/Template/Layout/printlayout.ctp' $dataForView = [ 'article_current' => object(App\Model\Entity\Article) { 'id' => (int) 21248, 'title' => 'A race towards climate catastrophe-Nagraj Adve', 'subheading' => '', 'description' => '<div align="justify"> -The Hindu </div> <p align="justify"> </p> <p align="justify"> </p> <p align="justify"> <em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em> </p> <p align="justify"> When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons. </p> <p align="justify"> <em>Impact on life cycles</em> </p> <p align="justify"> One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade. </p> <p align="justify"> This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species. </p> <p align="justify"> This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or "been the first groups in which whole species have gone extinct due to recent climate change." </p> <p align="justify"> Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that "if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that" ("Target Atmospheric CO: Where Should Humanity Aim?," The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org. </p> <p align="justify"> <em>Temperature regulator</em> </p> <p align="justify"> Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: "The similarity between CO and temperature in [the] Antarctica is jaw-dropping," a causal link he says that's even stronger than that between smoking and lung cancer, "kind of a gold standard in the medical world." Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience. </p> <p align="justify"> We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop. </p> <p align="justify"> <em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em> </p>', 'credit_writer' => 'The Hindu, 4 June, 2013, http://www.thehindu.com/opinion/op-ed/a-race-towards-climate-catastrophe/article4778996.ece', 'article_img' => '', 'article_img_thumb' => '', 'status' => (int) 1, 'show_on_home' => (int) 1, 'lang' => 'EN', 'category_id' => (int) 16, 'tag_keyword' => '', 'seo_url' => 'a-race-towards-climate-catastrophe-nagraj-adve-21393', 'meta_title' => null, 'meta_keywords' => null, 'meta_description' => null, 'noindex' => (int) 0, 'publish_date' => object(Cake\I18n\FrozenDate) {}, 'most_visit_section_id' => null, 'article_big_img' => null, 'liveid' => (int) 21393, 'created' => object(Cake\I18n\FrozenTime) {}, 'modified' => object(Cake\I18n\FrozenTime) {}, 'edate' => '', 'tags' => [ [maximum depth reached] ], 'category' => object(App\Model\Entity\Category) {}, '[new]' => false, '[accessible]' => [ [maximum depth reached] ], '[dirty]' => [[maximum depth reached]], '[original]' => [[maximum depth reached]], '[virtual]' => [[maximum depth reached]], '[hasErrors]' => false, '[errors]' => [[maximum depth reached]], '[invalid]' => [[maximum depth reached]], '[repository]' => 'Articles' }, 'articleid' => (int) 21248, 'metaTitle' => 'LATEST NEWS UPDATES | A race towards climate catastrophe-Nagraj Adve', 'metaKeywords' => 'Global Warming,climate change,Environment', 'metaDesc' => ' -The Hindu The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it...', 'disp' => '<div align="justify">-The Hindu</div><p align="justify"> </p><p align="justify"> </p><p align="justify"><em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em></p><p align="justify">When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons.</p><p align="justify"><em>Impact on life cycles</em></p><p align="justify">One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade.</p><p align="justify">This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species.</p><p align="justify">This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or "been the first groups in which whole species have gone extinct due to recent climate change."</p><p align="justify">Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that "if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that" ("Target Atmospheric CO: Where Should Humanity Aim?," The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org.</p><p align="justify"><em>Temperature regulator</em></p><p align="justify">Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: "The similarity between CO and temperature in [the] Antarctica is jaw-dropping," a causal link he says that's even stronger than that between smoking and lung cancer, "kind of a gold standard in the medical world." Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience.</p><p align="justify">We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop.</p><p align="justify"><em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em></p>', 'lang' => 'English', 'SITE_URL' => 'https://im4change.in/', 'site_title' => 'im4change', 'adminprix' => 'admin' ] $article_current = object(App\Model\Entity\Article) { 'id' => (int) 21248, 'title' => 'A race towards climate catastrophe-Nagraj Adve', 'subheading' => '', 'description' => '<div align="justify"> -The Hindu </div> <p align="justify"> </p> <p align="justify"> </p> <p align="justify"> <em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em> </p> <p align="justify"> When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons. </p> <p align="justify"> <em>Impact on life cycles</em> </p> <p align="justify"> One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade. </p> <p align="justify"> This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species. </p> <p align="justify"> This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or "been the first groups in which whole species have gone extinct due to recent climate change." </p> <p align="justify"> Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that "if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that" ("Target Atmospheric CO: Where Should Humanity Aim?," The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org. </p> <p align="justify"> <em>Temperature regulator</em> </p> <p align="justify"> Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: "The similarity between CO and temperature in [the] Antarctica is jaw-dropping," a causal link he says that's even stronger than that between smoking and lung cancer, "kind of a gold standard in the medical world." Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience. </p> <p align="justify"> We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop. </p> <p align="justify"> <em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em> </p>', 'credit_writer' => 'The Hindu, 4 June, 2013, http://www.thehindu.com/opinion/op-ed/a-race-towards-climate-catastrophe/article4778996.ece', 'article_img' => '', 'article_img_thumb' => '', 'status' => (int) 1, 'show_on_home' => (int) 1, 'lang' => 'EN', 'category_id' => (int) 16, 'tag_keyword' => '', 'seo_url' => 'a-race-towards-climate-catastrophe-nagraj-adve-21393', 'meta_title' => null, 'meta_keywords' => null, 'meta_description' => null, 'noindex' => (int) 0, 'publish_date' => object(Cake\I18n\FrozenDate) {}, 'most_visit_section_id' => null, 'article_big_img' => null, 'liveid' => (int) 21393, 'created' => object(Cake\I18n\FrozenTime) {}, 'modified' => object(Cake\I18n\FrozenTime) {}, 'edate' => '', 'tags' => [ (int) 0 => object(Cake\ORM\Entity) {}, (int) 1 => object(Cake\ORM\Entity) {}, (int) 2 => object(Cake\ORM\Entity) {} ], 'category' => object(App\Model\Entity\Category) {}, '[new]' => false, '[accessible]' => [ '*' => true, 'id' => false ], '[dirty]' => [], '[original]' => [], '[virtual]' => [], '[hasErrors]' => false, '[errors]' => [], '[invalid]' => [], '[repository]' => 'Articles' } $articleid = (int) 21248 $metaTitle = 'LATEST NEWS UPDATES | A race towards climate catastrophe-Nagraj Adve' $metaKeywords = 'Global Warming,climate change,Environment' $metaDesc = ' -The Hindu The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it...' $disp = '<div align="justify">-The Hindu</div><p align="justify"> </p><p align="justify"> </p><p align="justify"><em>The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre</em></p><p align="justify">When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons.</p><p align="justify"><em>Impact on life cycles</em></p><p align="justify">One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade.</p><p align="justify">This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species.</p><p align="justify">This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or "been the first groups in which whole species have gone extinct due to recent climate change."</p><p align="justify">Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that "if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that" ("Target Atmospheric CO: Where Should Humanity Aim?," The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org.</p><p align="justify"><em>Temperature regulator</em></p><p align="justify">Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: "The similarity between CO and temperature in [the] Antarctica is jaw-dropping," a causal link he says that's even stronger than that between smoking and lung cancer, "kind of a gold standard in the medical world." Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience.</p><p align="justify">We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop.</p><p align="justify"><em>(Nagraj Adve is an activist based in Delhi and works on issues connected with global warming)</em></p>' $lang = 'English' $SITE_URL = 'https://im4change.in/' $site_title = 'im4change' $adminprix = 'admin'
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A race towards climate catastrophe-Nagraj Adve |
-The Hindu
The Earth is now in uncharted territory as atmospheric carbon dioxide has shot past the 400 ppm mark. There is no more room for manoeuvre When Brian Lara scored a scintillating 400 not out in Antigua in April 2004, it seemed his score would remain unchallenged for the foreseeable future. But we now have another player on the scene who has scored 400, and threatens to go past that number effortlessly - carbon dioxide (CO); CO levels in the atmosphere touched 400 parts per million (ppm) on May 9. Its symbolic significance is huge, its actual import is even bigger, for three reasons. Impact on life cycles One, the recent pace at which CO levels have been rising to reach 400 ppm. When Charles Keeling [the world's leading authority on atmospheric greenhouse gas accumulation and climate science pioneer] began measuring atmospheric CO in March 1958, and through the 1960s, CO emissions were found to be rising at a little over half a ppm a year. The world economy was at a much lower level than today notwithstanding post-War growth, and carbon emissions were commensurately lower. By the late 1990s this had changed, spurred primarily, but not exclusively, by the shifting of manufacturing to China, and capitalism's desire to cut costs of energy inputs and labour. CO rise in the first decade of this century made the collective jaw of climate scientists drop. Despite the world economic crisis since 2007, annual carbon dioxide emissions from burning fossil fuels have been rising in recent years, to 32 billion tonnes (plus another four billion tonnes from deforestation and even more of other gases). Eight billion tonnes of CO in the atmosphere equals 1 ppm. So even though the Earth absorbs - is being forced to absorb - twice as much CO (roughly 17-18 billion tonnes a year currently) as it used to 50 years ago, atmospheric CO levels have been galloping three times as fast, at a little over two ppm a year for the last decade. This is 20,000 times the long-term natural rate at which carbon dioxide has gone into and out of the atmosphere as part of the carbon cycle. A consequence, usually rendered invisible as we tend to be so anthropocentric, is the oceans getting more acidic, with harmful effects on corals and some marine species. This pace of emissions and consequent warming is also making it increasingly difficult for ecosystems and species to adapt. A metasurvey by Prof. Camille Parmesan [University of Texas, Austin] of 866 published studies reported species across the world struggling to cope with disruptions in the life cycles of predators and prey, of insect pollinators and flowering plants. Birds are laying their first eggs earlier. As their habitat gets warmer, other species are trying to move away from the Equator or climb higher. Consequently, mountaintop and polar species have suffered contractions in their range or "been the first groups in which whole species have gone extinct due to recent climate change." Two, as we reach 400 ppm and beyond, we are going farther away from safe levels of CO. Albeit a minority view, but a growing one, safe has been deemed as 350 ppm or lower. In its first articulation in 2008, [leading climate scientist] James Hansen and others wrote that "if humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, ... CO will need to be reduced ... to at most 350 ppm, but likely less than that" ("Target Atmospheric CO: Where Should Humanity Aim?," The Open Atmospheric Science Journal, 2008, 2, pp. 217-31). This paper provides the intellectual basis for the worldwide campaign to reduce CO, headed by the organisation, 350.org. Temperature regulator Three, the influence of CO levels on the Earth's temperatures and hence climate over the past 50 million years should give us pause. In The Long Thaw (Princeton 2009), Professor David Archer, who works on the global carbon cycle at the University of Chicago, writes: "The similarity between CO and temperature in [the] Antarctica is jaw-dropping," a causal link he says that's even stronger than that between smoking and lung cancer, "kind of a gold standard in the medical world." Falling CO levels contributed to the formation of ice caps on the Antarctic 34 million years ago. As CO levels fell further, to roughly 240 ppm three million years ago, temperatures fell in their wake sufficiently for ice to form in the Arctic. That's why Arctic ice is now the first to go. I have not come across any work on the potential impact of ice-free Arctic summers on India's climate, but you can bet your last rupee they will be considerable. CO was also one of two big factors in the Earth moving in and out of Ice Age glacials over the past 2.5 million years. It is this regulator of the Earth's temperature that we have been shortsightedly fiddling with, and pushed beyond the realms of human experience. We don't want to go much beyond 400 ppm. CO has one quality of the other great batsman of the last 25 years - longevity. A significant portion of CO emitted remains in the atmosphere for several millennia. Climate change is also largely irreversible for a thousand years after emissions stop. (Nagraj Adve is an activist based in Delhi and works on issues connected with global warming) |