气候变化领域集成服务门户(CCPortal): Response and feedback of the Indian summer monsoon and the Southern Westerly Winds to a temperature contrast between the hemispheres during the last glacial

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DOI	10.1016/j.earscirev.2019.102917
	Response and feedback of the Indian summer monsoon and the Southern Westerly Winds to a temperature contrast between the hemispheres during the last glacial–interglacial transitional period
	Hong B.; Rabassa J.; Uchida M.; Hong Y.; Peng H.; Ding H.; Guo Q.; Yao H.
发表日期	2019
ISSN	0012-8904
卷号	197
英文摘要	The hypothesis that an interhemispheric thermal gradient, or a temperature contrast between the hemispheres (TCBH), drives shifts in the latitudinal position of the Intertropical Convergence Zone (ITCZ) and the Southern Westerly Winds (SWW) is considered one of the most important climate change mechanisms proposed in the last few decades. However, the controversy over the shifting magnitude and direction of the ITCZ and the SWW brings uncertainty to the hypothesis. Here, we further examine the shifting characteristics of the ITCZ and its relationship with the intensity variation of the Indian summer monsoon (ISM) based on synthesis and summary of previously published literature data. In particular, we evaluate regional distribution patterns of the dry and wet climatic changes in southern South America during the last glacial–interglacial transitional period, including the Heinrich event 1, the Antarctic Cold Reversal, and the Younger Dryas. The results show that in response to the Northern Hemisphere-wide cooling and the Southern Hemisphere-wide warming (the Northern Hemisphere-wide warming and the Southern Hemisphere-wide cooling) during the period, the ITCZ over the Asian and northern South American continents and the SWW shift poleward (equatorward), while the intensity of the ISM decreases (increases). However, the shifting characteristics of the ITCZ over the vast Pacific Ocean remain unclear, which implies that the relationship between the TCBH and the El Niño-Southern Oscillation in the tropical Pacific Ocean needs to be studied. In addition, there may be a relatively stable core region in the SWW. This core region is located in Central Patagonia at approximately 47°S, where the local climate is wetter during the all transition period, showing the continuous influence of the SWW on this region. The position shift of the SWW in response to the TCBH phase changes seems to behave as a swing process with an axis of approximately 47°S. The poleward swing of the SWW may trigger the self-repairing process of the global climate system after the catastrophic impacts of the meltwater, including the pulling effect of the enhanced upwelling on the Atlantic meridional overturning circulation, the influence of CO2 released from the deep sea, and the impact of the gradual strengthening of the ISM. These results support and reinforce the hypothesis that the TCBH drives global climate change, highlight the global teleconnection characteristics of the key physical processes in the Earth's climate system and the important role of the SWW in this teleconnection, and provide a basis for further simulating the climate connections in the two hemispheres, especially the impact of the SWW on the global climate change. © 2019 Elsevier B.V.
英文关键词	Earth system; ENSO; Interhemispheric thermal gradient; ITCZ; Meridional overturning circulation; Patagonia; Peat
语种	英语
scopus关键词	climate feedback; climate variation; glacial-interglacial cycle; meridional circulation; monsoon; paleoclimate; summer; temperature gradient; uncertainty analysis; westerly; wind field; Younger Dryas; South America
来源期刊	EARTH-SCIENCE REVIEWS
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/209833
作者单位	State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, 99 Lincheng Road West, Guiyang, Guizhou 550081, China; CAS Center for Excellence in Quaternary Science and Global Change, Xi'an, 710061, China; Centro Austral de Investigaciones Cientificas (CADIC, CONICET), C.C. 92, Ushuaia, Tierra del Fuego 9410, Argentina; Center for Environmental Measurement and Analysis, National Institute for Environmental Studies, Onogawa 16-2, Tsukuba, Ibaraki 305-0053, Japan
推荐引用方式 GB/T 7714	Hong B.,Rabassa J.,Uchida M.,等. Response and feedback of the Indian summer monsoon and the Southern Westerly Winds to a temperature contrast between the hemispheres during the last glacial–interglacial transitional period[J],2019,197.
APA	Hong B..,Rabassa J..,Uchida M..,Hong Y..,Peng H..,...&Yao H..(2019).Response and feedback of the Indian summer monsoon and the Southern Westerly Winds to a temperature contrast between the hemispheres during the last glacial–interglacial transitional period.EARTH-SCIENCE REVIEWS,197.
MLA	Hong B.,et al."Response and feedback of the Indian summer monsoon and the Southern Westerly Winds to a temperature contrast between the hemispheres during the last glacial–interglacial transitional period".EARTH-SCIENCE REVIEWS 197(2019).