{"id":6796,"date":"2019-06-05T14:00:34","date_gmt":"2019-06-05T18:00:34","guid":{"rendered":"http:\/\/sciencemediacentre.ca\/site\/?p=6796"},"modified":"2019-06-11T19:56:33","modified_gmt":"2019-06-11T23:56:33","slug":"l-nino-enhances-co2-uptake-by-north-american-vegetation","status":"publish","type":"post","link":"http:\/\/sciencemediacentre.ca\/site\/l-nino-enhances-co2-uptake-by-north-american-vegetation\/","title":{"rendered":"El Ni\u00f1o enhances CO<sub>2<\/sub> uptake by North American vegetation <img src=\"http:\/\/sciencemediacentre.ca\/site\/wp-content\/uploads\/2014\/01\/canada_flag_icon_small.gif\">"},"content":{"rendered":"<p><a href=\"https:\/\/advances.sciencemag.org\/content\/5\/6\/eaaw0076\" target=\"_blank\" rel=\"noopener noreferrer\"><em>Science Advances<\/em><\/a><br \/>\n<strong>Published June 5, 2019 | 14:00 EDT<\/strong><br \/>\nLong-term atmospheric CO<sub>2<\/sub> observations over North America document persistent responses to the El Ni\u00f1o\u2013Southern Oscillation, ocean climate influences. Increased water availability, warmer springs and cooler summers enhances carbon uptake over North America near and during El Ni\u00f1o. The increased uptake from North America partially offsets El Ni\u00f1o-driven increases in atmospheric carbon from the tropics.<\/p>\n<p><strong>Canadian co-author:<\/strong>\u00a0Doug Worthy, Environment and Climate Change Canada, Toronto &#8211;\u00a0<a href=\"mailto:doug.worthy@canada.ca\" target=\"_blank\" rel=\"noopener noreferrer\">doug.worthy@canada.ca<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Science Advances Published June 5, 2019 | 14:00 EDT Long-term atmospheric CO2 observations over North America document persistent responses to the El Ni\u00f1o\u2013Southern Oscillation, ocean climate influences. Increased water availability, warmer springs and cooler summers enhances carbon uptake over North America near and during El Ni\u00f1o. The increased uptake from North America partially offsets El [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_jetpack_newsletter_access":"","_jetpack_dont_email_post_to_subs":false,"_jetpack_newsletter_tier_id":0,"_jetpack_memberships_contains_paywalled_content":false,"_jetpack_memberships_contains_paid_content":false,"footnotes":""},"categories":[1327,3259,25],"tags":[],"class_list":["post-6796","post","type-post","status-publish","format-standard","hentry","category-article-scientifique","category-heads-up","category-paper-of-interest"],"jetpack_featured_media_url":"","jetpack_shortlink":"https:\/\/wp.me\/p4DqbN-1LC","jetpack_sharing_enabled":true,"_links":{"self":[{"href":"http:\/\/sciencemediacentre.ca\/site\/wp-json\/wp\/v2\/posts\/6796","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/sciencemediacentre.ca\/site\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"http:\/\/sciencemediacentre.ca\/site\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"http:\/\/sciencemediacentre.ca\/site\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"http:\/\/sciencemediacentre.ca\/site\/wp-json\/wp\/v2\/comments?post=6796"}],"version-history":[{"count":3,"href":"http:\/\/sciencemediacentre.ca\/site\/wp-json\/wp\/v2\/posts\/6796\/revisions"}],"predecessor-version":[{"id":6815,"href":"http:\/\/sciencemediacentre.ca\/site\/wp-json\/wp\/v2\/posts\/6796\/revisions\/6815"}],"wp:attachment":[{"href":"http:\/\/sciencemediacentre.ca\/site\/wp-json\/wp\/v2\/media?parent=6796"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/sciencemediacentre.ca\/site\/wp-json\/wp\/v2\/categories?post=6796"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/sciencemediacentre.ca\/site\/wp-json\/wp\/v2\/tags?post=6796"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}