globalchange  > 气候减缓与适应
DOI: 10.1002/2014GL061456
论文题名:
Surface warming hiatus caused by increased heat uptake across multiple ocean basins
作者: Drijfhout S.S.; Blaker A.T.; Josey S.A.; Nurser A.J.G.; Sinha B.; Balmaseda M.A.
刊名: Geophysical Research Letters
ISSN: 0094-9588
EISSN: 1944-9319
出版年: 2014
卷: 41, 期:22
起始页码: 7868
结束页码: 7874
语种: 英语
英文关键词: climate hiatus
Scopus关键词: Atmospheric temperature ; Heat losses ; Surface waters ; climate hiatus ; Different mechanisms ; Eastern pacific ; Global surface warming ; Ocean heat uptake ; Sea surface temperature (SST) ; Southern Annular Mode ; Subpolar North Atlantic ; Oceanography ; climate change ; global warming ; heat balance ; hiatus ; sea surface temperature ; Agulhas Current ; Atlantic Ocean ; Atlantic Ocean (Subtropical) ; Indian Ocean ; Pacific Ocean ; Pacific Ocean (East)
英文摘要: The first decade of the 21st century was characterized by a hiatus in global surface warming. Using ocean model hindcasts and reanalyses we show that heat uptake between the 1990s and 2000s increased by 0.7 ± 0.3W m-2. Approximately 30% of the increase is associated with colder sea surface temperatures in the eastern Pacific. Other basins contribute via reduced heat loss to the atmosphere, in particular, the Southern and subtropical Indian Oceans (30%) and the subpolar North Atlantic (40%). A different mechanism is important at longer timescales (1960s-present) over which the Southern Annular Mode trended upward. In this period, increased ocean heat uptake has largely arisen from reduced heat loss associated with reduced winds over the Agulhas Return Current and southward displacement of Southern Ocean westerlies. © 2014. American Geophysical Union. All Rights Reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84923306520&doi=10.1002%2f2014GL061456&partnerID=40&md5=3ce8574e5173aba792e94b784626c72a
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/6852
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作者单位: NOCS, University of Southampton, Southampton, United Kingdom

Recommended Citation:
Drijfhout S.S.,Blaker A.T.,Josey S.A.,et al. Surface warming hiatus caused by increased heat uptake across multiple ocean basins[J]. Geophysical Research Letters,2014-01-01,41(22).
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