聚类揭示欧亚大陆冬季大气阻塞与寒潮之间的关系

IF 3.8 2区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Zifan Yang, Wenyu Huang, Jonathon S. Wright, Wenqian Ma, Bin Wang
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引用次数: 0

摘要

利用基于模式相关性的统一聚类框架,确定了 1948-2021 年冬季(12 月至 3 月)欧亚大陆及周边海洋上空的八个阻塞体制。这些机制是根据其作用中心来标注的,它们分别位于西大西洋、格陵兰岛、东大西洋、斯堪的纳维亚半岛、乌拉尔山脉和西伯利亚、鄂霍次克海、白令海峡和北太平洋。值得注意的是,这种分类对时间段几乎不敏感,而主要取决于不同阻塞事件的百分比。在这八种机制中,寒潮的空间分布差异很大。主要由于阻塞活动中心下游的冷平流,在欧亚大陆的部分地区可以观测到寒潮。探讨了这八种阻塞机制与大规模气候变异模式(包括北极涛动、北大西洋涛动和厄尔尼诺-南方涛动)之间的可能关系。不仅讨论了当代联系,还讨论了大尺度模式的预测价值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Relationships Between the Wintertime Atmospheric Blocking and Cold Surges Over Eurasia Revealed by Clustering

A unified clustering framework based on pattern correlation is used to identify eight blocking regimes over Eurasia and surrounding oceans during the winter months (December–March) of 1948–2021. The regimes are labeled based on their centers of action, which are located over the West Atlantic, Greenland, the East Atlantic, Scandinavia, the Ural Mountains and Siberia, the Okhotsk Sea, the Bering Strait, and the North Pacific. It should be noted that the classification is almost insensitive to the time period but mainly depends on the percentage of different blocking events. The spatial distributions of cold surges differ substantially among these eight regimes. Due mainly to the cold advection downstream of the centers of blocking activities, cold surges can be observed over parts of the Eurasian continent. Possible relationships between the eight blocking regimes and large-scale modes of climate variability, including the Arctic Oscillation, the North Atlantic Oscillation, and the El Niño-Southern Oscillation, are explored. Not only contemporary connections but also the predictive value of large-scale modes is discussed.

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来源期刊
Journal of Geophysical Research: Atmospheres
Journal of Geophysical Research: Atmospheres Earth and Planetary Sciences-Geophysics
CiteScore
7.30
自引率
11.40%
发文量
684
期刊介绍: JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.
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