The global warming hiatus: Slowdown or redistribution?. Issue 11 (22nd November 2016)

• Record Type: Journal Article
• Authors: Yan, Xiao‐Hai; Boyer, Tim; Trenberth, Kevin; Karl, Thomas R.; Xie, Shang‐Ping; Nieves, Veronica; Tung, Ka‐Kit; Roemmich, Dean
• Is Part Of: Earth's future. Volume 4:Issue 11(2016)
• Page Start: 472
• Page End: 482
• Publication Date: 2016-11-22
• Subjects: Global warming hiatus -- Heat energy -- Ocean monitoring; Environmental sciences -- Periodicals; Environmental sciences; Periodicals; 550
• DOI: 10.1002/2016EF000417
• Languages: English
• ISSNs: 2328-4277

Abstract

Abstract: Global mean surface temperatures (GMST) exhibited a smaller rate of warming during 1998–2013, compared to the warming in the latter half of the 20th Century. Although, not a "true" hiatus in the strict definition of the word, this has been termed the "global warming hiatus" by IPCC (2013). There have been other periods that have also been defined as the "hiatus" depending on the analysis. There are a number of uncertainties and knowledge gaps regarding the "hiatus." This report reviews these issues and also posits insights from a collective set of diverse information that helps us understand what we do and do not know. One salient insight is that the GMST phenomenon is a surface characteristic that does not represent a slowdown in warming of the climate system but rather is an energy redistribution within the oceans. Improved understanding of the ocean distribution and redistribution of heat will help better monitor Earth's energy budget and its consequences. A review of recent scientific publications on the "hiatus" shows the difficulty and complexities in pinpointing the oceanic sink of the "missing heat" from the atmosphere and the upper layer of the oceans, which defines the "hiatus." Advances in "hiatus" research and outlooks (recommendations) are given in this report. Key Points: From 1998 to 2013, the rate of global mean surface warming slowed (some have termed this a global warming hiatus); we argue that this represents a redistribution of energy within the Earth system Natural, decadal variability plays a crucial role in the rate of global surface warming Improved understanding of ocean distribution and redistribution of heat will help us better monitor Earth energy budget and will maintain and increase ocean monitoring