气候变化领域集成服务门户(CCPortal): Different enhancement of the east Asian summer monsoon under global warming and interglacial epochs simulated by CMIP6 models: Role of the subtropical high

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DOI	10.1175/JCLI-D-20-0304.1
	Different enhancement of the east Asian summer monsoon under global warming and interglacial epochs simulated by CMIP6 models: Role of the subtropical high
	He C.; Zhou W.
发表日期	2020
ISSN	0894-8755
起始页码	9721
结束页码	9733
卷号	33 期号:22
英文摘要	Southerly wind in the lower troposphere is an essential feature of East Asian summer monsoon (EASM) circulation, which is reported to be enhanced under global warming scenarios and interglacial epochs. Based on an analysis of an ensemble of CMIP6 models, this study shows that the magnitude of intensification of the EASM circulation is much smaller under global warming scenarios than during interglacial epochs. Distinct changes in the western North Pacific subtropical high (WNPSH) are responsible for the different responses of the EASM circulation. The WNPSH is substantially enhanced during interglacial epochs, which acts to strengthen the southerly wind associated with the EASM on the western flank of the WNPSH. However, the change in the WNPSH is insignificant and cannot strengthen the EASM under global warming scenarios, and the weakly enhanced EASM circulation may be a direct response to intensified heating over the Tibetan Plateau. The land–ocean thermal contrast explains the different responses of the WNPSH. During interglacial epochs, the summertime surface warming over the subtropical North Pacific is much weaker than over Eurasia due to the large thermal inertia of the ocean to increased insolation, and the WNPSH is intensified as a response to the suppressed latent heating over the subtropical North Pacific. The fast response of the WNPSH to abrupt quadrupling of CO2 without sufficient ocean warming is an analog to the interglacial epochs, but it is offset by the effect of slow oceanic warming, resulting in an insignificant change of the WNPSH under global warming scenarios. © 2020 American Meteorological Society.
英文关键词	Atmospheric thermodynamics; Tropics; East Asian summer monsoon; Essential features; Interglacial epochs; Lower troposphere; Surface warming; Thermal inertia; Tibetan Plateau; Western North Pacific; Global warming; atmospheric circulation; atmospheric modeling; CMIP; global warming; interglacial; monsoon; summer; troposphere; China; Qinghai-Xizang Plateau
语种	英语
来源期刊	Journal of Climate
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/171044
作者单位	Institute for Environmental and Climate Research, Jinan University, Guangzhou, China; Guy Carpenter Asia-Pacific Climate Impact Centre, School of Energy and Environment, City University of Hong Kong, Hong Kong, Hong Kong
推荐引用方式 GB/T 7714	He C.,Zhou W.. Different enhancement of the east Asian summer monsoon under global warming and interglacial epochs simulated by CMIP6 models: Role of the subtropical high[J],2020,33(22).
APA	He C.,&Zhou W..(2020).Different enhancement of the east Asian summer monsoon under global warming and interglacial epochs simulated by CMIP6 models: Role of the subtropical high.Journal of Climate,33(22).
MLA	He C.,et al."Different enhancement of the east Asian summer monsoon under global warming and interglacial epochs simulated by CMIP6 models: Role of the subtropical high".Journal of Climate 33.22(2020).