Robust Asymmetry of the Future Arctic Polar Vortex Is Driven by Tropical Pacific Warming
The future stratosphere is globally dominated by a strong radiative cooling due to the increase in greenhouse gases. However, we find that over North America, the Arctic stratospheric cooling is suppressed or rather warming occurs, whereas over Eurasia stratospheric cooling is most pronounced, leadi...
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Online Access: | http://hdl.handle.net/2115/83557 https://doi.org/10.1029/2021GL093440 |
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fthokunivhus:oai:eprints.lib.hokudai.ac.jp:2115/83557 2023-05-15T13:14:57+02:00 Robust Asymmetry of the Future Arctic Polar Vortex Is Driven by Tropical Pacific Warming Matsumura, Shinji Yamazaki, Koji Horinouchi, Takeshi http://hdl.handle.net/2115/83557 https://doi.org/10.1029/2021GL093440 eng eng American Geophysical Union http://hdl.handle.net/2115/83557 Geophysical Research Letters, 48(11): e2021GL093440 http://dx.doi.org/10.1029/2021GL093440 Copyright 2021 American Geophysical Union. stratospheric polar vortex climate change North American stratospheric warming Tropical Pacific warming 451 article fthokunivhus https://doi.org/10.1029/2021GL093440 2022-11-18T01:06:31Z The future stratosphere is globally dominated by a strong radiative cooling due to the increase in greenhouse gases. However, we find that over North America, the Arctic stratospheric cooling is suppressed or rather warming occurs, whereas over Eurasia stratospheric cooling is most pronounced, leading to an asymmetric polar vortex, based on 21st century climate model simulations. There are many causes that drive polar vortex variability, which make future projections highly uncertain. Our model simulations demonstrate that tropical warming induces the asymmetric polar vortex. The eastern equatorial Pacific warming causes eastward-shifted teleconnection with a deepened Aleutian low, which strengthens the polar vortex over Eurasia and weakens over North America by enhancing the vertical wave propagation into the stratosphere. The asymmetric polar vortex is projected to markedly develop in the 2030s, and so could affect winter surface climate over mid- to high-latitudes of Eurasia in the near future. Article in Journal/Newspaper aleutian low Arctic Climate change Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) Arctic Pacific Geophysical Research Letters 48 11 |
institution |
Open Polar |
collection |
Hokkaido University Collection of Scholarly and Academic Papers (HUSCAP) |
op_collection_id |
fthokunivhus |
language |
English |
topic |
stratospheric polar vortex climate change North American stratospheric warming Tropical Pacific warming 451 |
spellingShingle |
stratospheric polar vortex climate change North American stratospheric warming Tropical Pacific warming 451 Matsumura, Shinji Yamazaki, Koji Horinouchi, Takeshi Robust Asymmetry of the Future Arctic Polar Vortex Is Driven by Tropical Pacific Warming |
topic_facet |
stratospheric polar vortex climate change North American stratospheric warming Tropical Pacific warming 451 |
description |
The future stratosphere is globally dominated by a strong radiative cooling due to the increase in greenhouse gases. However, we find that over North America, the Arctic stratospheric cooling is suppressed or rather warming occurs, whereas over Eurasia stratospheric cooling is most pronounced, leading to an asymmetric polar vortex, based on 21st century climate model simulations. There are many causes that drive polar vortex variability, which make future projections highly uncertain. Our model simulations demonstrate that tropical warming induces the asymmetric polar vortex. The eastern equatorial Pacific warming causes eastward-shifted teleconnection with a deepened Aleutian low, which strengthens the polar vortex over Eurasia and weakens over North America by enhancing the vertical wave propagation into the stratosphere. The asymmetric polar vortex is projected to markedly develop in the 2030s, and so could affect winter surface climate over mid- to high-latitudes of Eurasia in the near future. |
format |
Article in Journal/Newspaper |
author |
Matsumura, Shinji Yamazaki, Koji Horinouchi, Takeshi |
author_facet |
Matsumura, Shinji Yamazaki, Koji Horinouchi, Takeshi |
author_sort |
Matsumura, Shinji |
title |
Robust Asymmetry of the Future Arctic Polar Vortex Is Driven by Tropical Pacific Warming |
title_short |
Robust Asymmetry of the Future Arctic Polar Vortex Is Driven by Tropical Pacific Warming |
title_full |
Robust Asymmetry of the Future Arctic Polar Vortex Is Driven by Tropical Pacific Warming |
title_fullStr |
Robust Asymmetry of the Future Arctic Polar Vortex Is Driven by Tropical Pacific Warming |
title_full_unstemmed |
Robust Asymmetry of the Future Arctic Polar Vortex Is Driven by Tropical Pacific Warming |
title_sort |
robust asymmetry of the future arctic polar vortex is driven by tropical pacific warming |
publisher |
American Geophysical Union |
url |
http://hdl.handle.net/2115/83557 https://doi.org/10.1029/2021GL093440 |
geographic |
Arctic Pacific |
geographic_facet |
Arctic Pacific |
genre |
aleutian low Arctic Climate change |
genre_facet |
aleutian low Arctic Climate change |
op_relation |
http://hdl.handle.net/2115/83557 Geophysical Research Letters, 48(11): e2021GL093440 http://dx.doi.org/10.1029/2021GL093440 |
op_rights |
Copyright 2021 American Geophysical Union. |
op_doi |
https://doi.org/10.1029/2021GL093440 |
container_title |
Geophysical Research Letters |
container_volume |
48 |
container_issue |
11 |
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1766266234614054912 |