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...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2023
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Subjects: | |
Online Access: | https://doi.org/10.1029/2023GL105180 https://doaj.org/article/40a5868c2c234bddba43dfd372a2e66f |
_version_ | 1821799075190669312 |
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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 |
genre_facet | Arctic Global warming |
geographic | Arctic |
geographic_facet | Arctic |
id | ftdoajarticles:oai:doaj.org/article:40a5868c2c234bddba43dfd372a2e66f |
institution | Open Polar |
language | English |
op_collection_id | ftdoajarticles |
op_doi | https://doi.org/10.1029/2023GL105180 |
op_relation | 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 |
op_source | Geophysical Research Letters, Vol 50, Iss 22, Pp n/a-n/a (2023) |
publishDate | 2023 |
publisher | Wiley |
record_format | openpolar |
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 |