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DOI10.1175/JCLI-D-20-0298.1
A bridging role of winter snow over Northern China and Southern Mongolia in linking the east Asian winter and summer monsoons
Lu M.; Kuang Z.; Yang S.; Li Z.; Fan H.
发表日期2020
ISSN0894-8755
起始页码9849
结束页码9862
卷号33期号:22
英文摘要Eurasian snow, one of the most important factors that influence the Asian monsoons, has long been viewed as a useful predictor for seasonal monsoon prediction. In this study, observations and model simulations are used to demonstrate a bridging role of the winter snow anomaly over northern China and southern Mongolia (NCSM) in the relationship between the East Asian winter monsoon (EAWM) and the East Asian summer monsoon (EASM). Enhanced snow in NCSM results in local surface and tropospheric cooling, strengthening the EAWM through cold-air intrusion induced by northerly wind anomalies. In turn, the stronger EAWM provides a favorable condition for enhanced snowfall over East Asia to the south, indicating an active snow–EAWM interaction. The continental cooling could be maintained until summer due to the memory effect of snowmelt and moistening as well as the snow–monsoon interaction in the spring, causing changes in the meridional temperature gradient and associated upper-level westerlies in the summer. The interaction between the strengthened westerlies over the northern Tibetan Plateau and the topography of the plateau could lead to anomalous downstream convergence and compensating divergence to the south. Therefore, anomalous cyclonic circulation and increased rainfall occur over northeastern China and the Korean Peninsula, but anticyclonic circulation and decreased rainfall appear over the subtropical East Asia–Pacific region. Moreover, limited analysis shows that, compared to sea surface temperature feedback, the direct impact of snow anomaly on the EAWM–EASM connection seems more important. © 2020 American Meteorological Society.
英文关键词Atmospheric thermodynamics; Oceanography; Rain; Surface waters; Topography; Anticyclonic circulation; Cyclonic circulation; East Asian summer monsoon; East Asian winter monsoon; Favorable conditions; Meridional temperature gradient; Northern Tibetan plateaux; Sea surface temperature (SST); Snow; anticyclone; climate change; monsoon; summer; weather forecasting; winter; China; Mongolia; 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/171046
作者单位School of Atmospheric Sciences, Sun Yat-sen University, Guangzhou, China; Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA, United States; School of Atmospheric Sciences, Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies, Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Guangdong, China; Institute of Environment, Energy and Sustainability, Chinese University of Hong Kong, Hong Kong, Hong Kong
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Lu M.,Kuang Z.,Yang S.,et al. A bridging role of winter snow over Northern China and Southern Mongolia in linking the east Asian winter and summer monsoons[J],2020,33(22).
APA Lu M.,Kuang Z.,Yang S.,Li Z.,&Fan H..(2020).A bridging role of winter snow over Northern China and Southern Mongolia in linking the east Asian winter and summer monsoons.Journal of Climate,33(22).
MLA Lu M.,et al."A bridging role of winter snow over Northern China and Southern Mongolia in linking the east Asian winter and summer monsoons".Journal of Climate 33.22(2020).
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