[口头报告]Influence of Arctic sea ice and Interdecadal Pacific Oscillation on the recent increase of winter extreme snowfall in Northeast China

Influence of Arctic sea ice and Interdecadal Pacific Oscillation on the recent increase of winter extreme snowfall in Northeast China
编号:444 稿件编号:57 访问权限:仅限参会人 更新:2024-04-10 20:04:03 浏览:441次 口头报告

报告开始:2024年05月19日 14:40 (Asia/Shanghai)

报告时间:12min

所在会议:[S12] 主题12、大气物理与气象气候 » [S12-9] 主题12、大气物理与气象气候 专题12.9(19日下午,226)

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摘要
In recent decades, Northeast China (NEC) has witnessed a substantial 20% rise in the occurrence of intense winter snowfall, resulting in a notable increase in the overall snowfall accumulation. Using Empirical Orthogonal Function (EOF) analysis, this study identifies a dominant interdecadal variation of the winter extreme snowfall with a turning point around 2000. The analysis uncovers abnormal atmospheric circulations linked to the positive phase of the like-Scandinavian pattern and anomalous North Pacific anticyclone, providing favorable conditions for cold air outbreak and water vapor enhancement for the increase in extreme snowfall. The positive phase of the like-Scandinavian pattern exhibits a strong correlation with sea ice loss in the Baffin Bay, Greenland Sea, and Barents-Kara Sea (BGBK). This positive pattern is primarily sustained by a positive feedback mechanism stemming from sea-ice-atmosphere interactions. Specifically, the positive like-Scandinavian pattern leads to increased water vapor over the BGBK region, promoting sea ice loss through enhanced clear-sky downward longwave radiation (CDLW) and increased surface turbulent heat flux. Conversely, a positive sea surface temperature anomaly prevails in the negative phase of the Interdecadal Pacific Oscillation (IPO), triggering an anomalous anticyclone over the North Pacific and East Asia, contributing to the observed increase in extreme snowfall over NEC. Furthermore, this study demonstrates a modulating relationship between the positive like-Scandinavian pattern and the anomalous anticyclone associated with the negative phase of the IPO, achieved through the triggering of Rossby wave trains, which were verified through numerical experiments using an atmospheric general circulation model. These results underscore the joint impact of interdecadal variability in Arctic Sea ice and the IPO on the decadal increase in winter extreme snowfall over NEC.
关键字
Extreme snowfall,Arctic Sea ice,Interdecadal Pacific Oscillation,Sea-ice-atmosphere interaction,Northeast China
报告人
高凯伦
高级工程师 北京市气候中心

稿件作者
高凯伦 北京市气候中心
汤雨恒 中国科学院大气物理研究所
ChenDeliang 哥德堡大学
王冀 北京市气候中心
段安民 厦门大学
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