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北极与欧亚大陆地表气温之间的亚季节关系。

Subseasonal relationship between Arctic and Eurasian surface air temperature.

作者信息

Kim Hye-Jin, Son Seok-Woo, Moon Woosok, Kug Jong-Seong, Hwang Jaeyoung

机构信息

School of Earth and Environmental Sciences, Seoul National University, Gwanak-ro, Gwanak-gu, Seoul, 08826, South Korea.

Department of Mathematics, Stockholm University, Stockholm, Sweden.

出版信息

Sci Rep. 2021 Feb 18;11(1):4081. doi: 10.1038/s41598-021-83486-5.

DOI:10.1038/s41598-021-83486-5
PMID:33603052
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7892886/
Abstract

The subseasonal relationship between Arctic and Eurasian surface air temperature (SAT) is re-examined using reanalysis data. Consistent with previous studies, a significant negative correlation is observed in cold season from November to February, but with a local minimum in late December. This relationship is dominated not only by the warm Arctic-cold Eurasia (WACE) pattern, which becomes more frequent during the last two decades, but also by the cold Arctic-warm Eurasia (CAWE) pattern. The budget analyses reveal that both WACE and CAWE patterns are primarily driven by the temperature advection associated with sea level pressure anomaly over the Ural region, partly cancelled by the diabatic heating. It is further found that, although the anticyclonic anomaly of WACE pattern mostly represents the Ural blocking, about 20% of WACE cases are associated with non-blocking high pressure systems. This result indicates that the Ural blocking is not a necessary condition for the WACE pattern, highlighting the importance of transient weather systems in the subseasonal Arctic-Eurasian SAT co-variability.

摘要

利用再分析数据重新审视了北极与欧亚大陆地表气温(SAT)之间的亚季节关系。与之前的研究一致,在11月至2月的寒冷季节观察到显著的负相关,但在12月下旬出现局部最小值。这种关系不仅由暖北极 - 冷欧亚(WACE)模式主导,该模式在过去二十年中变得更加频繁,还由冷北极 - 暖欧亚(CAWE)模式主导。预算分析表明,WACE和CAWE模式主要由与乌拉尔地区海平面气压异常相关的温度平流驱动,部分被非绝热加热抵消。进一步发现,尽管WACE模式的反气旋异常大多代表乌拉尔阻塞,但约20%的WACE情况与非阻塞高压系统有关。这一结果表明,乌拉尔阻塞不是WACE模式的必要条件,突出了瞬变天气系统在亚季节北极 - 欧亚SAT共变率中的重要性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0a5a/7892886/73f67a822429/41598_2021_83486_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0a5a/7892886/a7c930830543/41598_2021_83486_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0a5a/7892886/c908e8e995b1/41598_2021_83486_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0a5a/7892886/0c436ad0355e/41598_2021_83486_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0a5a/7892886/219f2bae054e/41598_2021_83486_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0a5a/7892886/73f67a822429/41598_2021_83486_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0a5a/7892886/a7c930830543/41598_2021_83486_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0a5a/7892886/c908e8e995b1/41598_2021_83486_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0a5a/7892886/0c436ad0355e/41598_2021_83486_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0a5a/7892886/219f2bae054e/41598_2021_83486_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0a5a/7892886/73f67a822429/41598_2021_83486_Fig5_HTML.jpg

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本文引用的文献

1
Arctic-Eurasian climate linkage induced by tropical ocean variability.北极-欧亚气候的联系由热带海洋变化引起。
Nat Commun. 2019 Aug 1;10(1):3441. doi: 10.1038/s41467-019-11359-7.
2
Vertical Feedback Mechanism of Winter Arctic Amplification and Sea Ice Loss.冬季北极放大效应与海冰损失的垂直反馈机制
Sci Rep. 2019 Feb 4;9(1):1184. doi: 10.1038/s41598-018-38109-x.
3
A stratospheric pathway linking a colder Siberia to Barents-Kara Sea sea ice loss.一条连接更寒冷的西伯利亚与巴伦支海-喀拉海海冰流失的平流层路径。
Sci Adv. 2018 Jul 25;4(7):eaat6025. doi: 10.1126/sciadv.aat6025. eCollection 2018 Jul.
4
Weakening of the stratospheric polar vortex by Arctic sea-ice loss.北极海冰减少导致平流层极地涡旋减弱。
Nat Commun. 2014 Sep 2;5:4646. doi: 10.1038/ncomms5646.