中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Multidecadal Changes of the Upper Indian Ocean Heat Content during 1965-2016

文献类型:期刊论文

作者Li, Yuanlong1,2,3; Han, Weiqing2; Hu, Aixue4; Meehl, Gerald A.4; Wang, Fan1,5,6
刊名JOURNAL OF CLIMATE
出版日期2018-10-01
卷号31期号:19页码:7863-7884
ISSN号0894-8755
关键词Indian Ocean Ocean circulation Wind stress Pacific decadal oscillation Multidecadal variability
DOI10.1175/JCLI-D-18-0116.1
英文摘要Ocean heat uptake is the primary heat sink of the globe and modulates its surface warming rate. In situ observations during the past half century documented obvious multidecadal variations in the upper-ocean heat content (0-400 m; OHC400) of the Indian Ocean (IO). The observed OHC400 showed an increase of (5.9 +/- 2.5) x 10(21) J decade(-1) during 1965-79, followed by a decrease of (-5.2 +/- 2.5) x 10(21) J decade(-1) during 1980-96, and a rapid increase of (13.6 +/- 1.1) x 10(21) J decade(-1) during 2000-14. These variations are faithfully reproduced by an Indo-Pacific simulation of an ocean general circulation model (OGCM), and insights into the underlying mechanisms are gained through OGCM experiments. The Pacific wind forcing through the Indonesian Throughflow (ITF) was the leading driver of the basin-integrated OHC400 increase during 1965-79 and the decrease during 1980-96, whereas after 2000 local wind and heat flux forcing within the IO made a larger contribution. The ITF heat transport is primarily dictated by Pacific trade winds. It directly affects the south IO, after which the signatures can enter the north IO through the meridional heat transport of the western boundary current. The prevailing warming of the western-to-central IO for 2000-14 was largely induced by equatorial easterly wind trends, Ekman downwelling off the equator, and northeasterly wind trends over the west Asia-East Africa coastal region. The increasing downward longwave radiation, probably reflecting anthropogenic greenhouse gas forcing, overcame the decreasing surface shortwave radiation and also made a significant contribution to the rapid upper-IO warming after 2000.
WOS关键词SEA-SURFACE TEMPERATURE ; INTERDECADAL PACIFIC OSCILLATION ; SHALLOW OVERTURNING CIRCULATION ; GLOBAL-WARMING HIATUS ; ANTHROPOGENIC AEROSOLS ; CLIMATE SYSTEM ; INDONESIAN THROUGHFLOW ; DECADAL VARIABILITY ; REANALYSIS PROJECT ; ATMOSPHERIC BRIDGE
资助项目National Natural Science Foundation of China (NSFC)[41776001] ; National Program on Global Change and Air-Sea Interaction[GASI-IPOVAI-01-01] ; AoShan Talents Program ; Qingdao National Laboratory for Marine Science and Technology (Grant 2015ASTP) ; NSF-AGS[1446480] ; NSF-OCE[1658132]
WOS研究方向Meteorology & Atmospheric Sciences
语种英语
出版者AMER METEOROLOGICAL SOC
WOS记录号WOS:000442201100001
资助机构National Natural Science Foundation of China (NSFC) ; National Program on Global Change and Air-Sea Interaction ; AoShan Talents Program ; Qingdao National Laboratory for Marine Science and Technology (Grant 2015ASTP) ; NSF-AGS ; NSF-OCE
源URL[http://ir.qibebt.ac.cn/handle/337004/12066]  
专题中国科学院青岛生物能源与过程研究所
通讯作者Li, Yuanlong
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China
2.Univ Colorado, Dept Atmospher & Ocean Sci, Boulder, CO 80309 USA
3.Qingdao Natl Lab Marine Sci & Technol, Funct Lab Ocean Dynam & Climate, Qingdao, Peoples R China
4.Natl Ctr Atmospher Res, POB 3000, Boulder, CO 80307 USA
5.Chinese Acad Sci, Qingdao Natl Lab Marine Sci & Technol, Funct Lab Ocean Dynam & Climate, Qingdao, Peoples R China
6.Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao, Peoples R China
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GB/T 7714
Li, Yuanlong,Han, Weiqing,Hu, Aixue,et al. Multidecadal Changes of the Upper Indian Ocean Heat Content during 1965-2016[J]. JOURNAL OF CLIMATE,2018,31(19):7863-7884.
APA Li, Yuanlong,Han, Weiqing,Hu, Aixue,Meehl, Gerald A.,&Wang, Fan.(2018).Multidecadal Changes of the Upper Indian Ocean Heat Content during 1965-2016.JOURNAL OF CLIMATE,31(19),7863-7884.
MLA Li, Yuanlong,et al."Multidecadal Changes of the Upper Indian Ocean Heat Content during 1965-2016".JOURNAL OF CLIMATE 31.19(2018):7863-7884.

入库方式: OAI收割

来源:青岛生物能源与过程研究所

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