Arctic Warming and Eurasian Cooling: Weakening and Reemergence

Abstract The observed Eurasian winter surface cooling from the 1990s to the early 2010s, which is contrary to global warming, has been extensively studied. Previous studies revealed that the surface cooling trend has significantly weakened in the past decade. Based on large‐ensemble simulations, thi...

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Published in:Geophysical Research Letters
Main Authors: Xinping Xu, Shengping He, Botao Zhou, Huijun Wang, Bo Sun
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2023GL105180
https://doaj.org/article/40a5868c2c234bddba43dfd372a2e66f
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author Xinping Xu
Shengping He
Botao Zhou
Huijun Wang
Bo Sun
author_facet Xinping Xu
Shengping He
Botao Zhou
Huijun Wang
Bo Sun
author_sort Xinping Xu
collection Directory of Open Access Journals: DOAJ Articles
container_issue 22
container_title Geophysical Research Letters
container_volume 50
description Abstract The observed Eurasian winter surface cooling from the 1990s to the early 2010s, which is contrary to global warming, has been extensively studied. Previous studies revealed that the surface cooling trend has significantly weakened in the past decade. Based on large‐ensemble simulations, this study reveals that the weakening of Eurasian surface cooling is primarily driven by the atmospheric internal variability, which coincides with the weakening of Arctic mid‐tropospheric warming and Eurasian mid‐tropospheric cooling. Negative Arctic Oscillation (−AO) and Ural blocking (UB) in combination dominate the intensity of Arctic mid‐tropospheric warming and Eurasian mid‐tropospheric cooling. In the future, there is a possibility that the severe Eurasian cooling trend with comparable magnitude to that during 1990–2013 may reemerge accompanied with Arctic mid‐tropospheric warming, in response to the decadal strengthening of −AO and UB. This may occur before the 2050s, when the atmospheric internal variability is able to overwhelm the effects of greenhouse gases.
format Article in Journal/Newspaper
genre Arctic
Global warming
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Global warming
geographic Arctic
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op_doi https://doi.org/10.1029/2023GL105180
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doi:10.1029/2023GL105180
https://doaj.org/article/40a5868c2c234bddba43dfd372a2e66f
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spelling ftdoajarticles:oai:doaj.org/article:40a5868c2c234bddba43dfd372a2e66f 2025-01-16T20:03:12+00:00 Arctic Warming and Eurasian Cooling: Weakening and Reemergence Xinping Xu Shengping He Botao Zhou Huijun Wang Bo Sun 2023-11-01T00:00:00Z https://doi.org/10.1029/2023GL105180 https://doaj.org/article/40a5868c2c234bddba43dfd372a2e66f EN eng Wiley https://doi.org/10.1029/2023GL105180 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2023GL105180 https://doaj.org/article/40a5868c2c234bddba43dfd372a2e66f Geophysical Research Letters, Vol 50, Iss 22, Pp n/a-n/a (2023) Arctic mid‐tropospheric warming Eurasian cooling Arctic Oscillation Ural blocking future projections Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2023GL105180 2024-08-05T17:49:23Z Abstract The observed Eurasian winter surface cooling from the 1990s to the early 2010s, which is contrary to global warming, has been extensively studied. Previous studies revealed that the surface cooling trend has significantly weakened in the past decade. Based on large‐ensemble simulations, this study reveals that the weakening of Eurasian surface cooling is primarily driven by the atmospheric internal variability, which coincides with the weakening of Arctic mid‐tropospheric warming and Eurasian mid‐tropospheric cooling. Negative Arctic Oscillation (−AO) and Ural blocking (UB) in combination dominate the intensity of Arctic mid‐tropospheric warming and Eurasian mid‐tropospheric cooling. In the future, there is a possibility that the severe Eurasian cooling trend with comparable magnitude to that during 1990–2013 may reemerge accompanied with Arctic mid‐tropospheric warming, in response to the decadal strengthening of −AO and UB. This may occur before the 2050s, when the atmospheric internal variability is able to overwhelm the effects of greenhouse gases. Article in Journal/Newspaper Arctic Global warming Directory of Open Access Journals: DOAJ Articles Arctic Geophysical Research Letters 50 22
spellingShingle Arctic mid‐tropospheric warming
Eurasian cooling
Arctic Oscillation
Ural blocking
future projections
Geophysics. Cosmic physics
QC801-809
Xinping Xu
Shengping He
Botao Zhou
Huijun Wang
Bo Sun
Arctic Warming and Eurasian Cooling: Weakening and Reemergence
title Arctic Warming and Eurasian Cooling: Weakening and Reemergence
title_full Arctic Warming and Eurasian Cooling: Weakening and Reemergence
title_fullStr Arctic Warming and Eurasian Cooling: Weakening and Reemergence
title_full_unstemmed Arctic Warming and Eurasian Cooling: Weakening and Reemergence
title_short Arctic Warming and Eurasian Cooling: Weakening and Reemergence
title_sort arctic warming and eurasian cooling: weakening and reemergence
topic Arctic mid‐tropospheric warming
Eurasian cooling
Arctic Oscillation
Ural blocking
future projections
Geophysics. Cosmic physics
QC801-809
topic_facet Arctic mid‐tropospheric warming
Eurasian cooling
Arctic Oscillation
Ural blocking
future projections
Geophysics. Cosmic physics
QC801-809
url https://doi.org/10.1029/2023GL105180
https://doaj.org/article/40a5868c2c234bddba43dfd372a2e66f