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Miêu tả
Miêu tảGlobalWarmingOceanHeatContent.jpg
English: Timeline from peer reviewed science paper (Comment on Ocean heat content and Earth's radiation imbalance. II. Relation to climate shifts Dana Nuccitelli, Robert Way, Rob Painting, John Church & John Cook ; March 31, 2012), showing how much of the heat added to the climate system went into the combination of land-ice-atmosphere, compared to the upper and lower oceans. According to this publication, overall there was no "pause" in global warming, even if the rate at which surface temperatures were increasing did slow down. Source: Skeptical Science
Français : Evolution temporelle (selon un article (Comment on Ocean heat content and Earth's radiation imbalance. II. Relation to climate shifts Dana Nuccitelli, Robert Way, Rob Painting, John Church & John Cook ; March 31, 2012) publiée par une revue scientifique à comité de lecture (c'est à dire examiné par des pairs), relatif à la part de chaleur ajoutée au système climatique et au transfert de cette chaleur supplémentaire vers le système terre-glace-atmosphère (en distinguant les compartiments océanique supérieur et profond). Selon cette publication, il n'y a pas eu globalement de "pause" dans le réchauffement climatique global, même quand l'augmentation des températures de l'air ou de surface ralentissait). Cet article était une réponse à un autre article (Douglass, D. H., & Knox, R. S. (2012). Ocean heat content and Earthʼs radiation imbalance. II. Relation to climate shifts. Physics Letters A, 376(14), 1226-1229., faisant lui-même suite à un premier article : Douglass, D. H., & Knox, R. S. (2009). Ocean heat content and Earth's radiation imbalance. Physics Letters A, 373(36), 3296-3300.), article qui concluait à une pause dans le réchauffement en négligeant de prendre en compte l'augmentation de température à grande profondeur). En tenant compte de ce facteur, la majorité des déséquilibres radiatifs décrits par l'article de Douglass & Knox (par rapport aux articles précédents) peut être expliquée, et les données redeviennent compatibles avec la poursuite d'un changement et réchauffement climatique global d'origine anthropique. Source: Skeptical Science, sous licence cc-by-sa
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English: Also published in the science literature. Nuccitelli, et al, "“Ocean heat content and Earthʼs radiation imbalance. II. Relation to climate shifts”, Physics Letters A, Volume 376, Issue 45, 1 October 2012, Pages 3466–3468; Authors' blog about the paper can be found at http://skepticalscience.com/nuccitelli-et-al-2012.html.
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