Projection of extreme precipitation induced by Arctic amplification over the Northern Hemisphere

Numerous attempts have been made to understand the connection between extreme weather and Arctic amplification (AA), and it is still disputed whether the mechanism is the elongation and deceleration of planetary-scale waves. In this study, we provide further evidence that the Arctic’s rapid warming...

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Main Authors: Jun Liu, Dongyou Wu, Xuanye Xu, Mingxia Ji, Quanliang Chen, Xin Wang
Format: Article
Language:English
Published: IOP Publishing 2021-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/ac0acc
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author Jun Liu
Dongyou Wu
Xuanye Xu
Mingxia Ji
Quanliang Chen
Xin Wang
author_facet Jun Liu
Dongyou Wu
Xuanye Xu
Mingxia Ji
Quanliang Chen
Xin Wang
author_sort Jun Liu
collection DOAJ
description Numerous attempts have been made to understand the connection between extreme weather and Arctic amplification (AA), and it is still disputed whether the mechanism is the elongation and deceleration of planetary-scale waves. In this study, we provide further evidence that the Arctic’s rapid warming is influencing extreme precipitation in the Northern Hermisphere based on observation and model outputs, and elucidate the underlying dynamic mechanisms. We find that AA has a significant positive correlation with extreme precipitation, both in the past (1901–2018) and in the future (by 2100). Moreover, observations reveal that, with the enhancement of AA since the mid-1980s, the planetary-scale wave amplitude has increased significantly at 0.66°/decade. This is associated with a negative Northern Hemisphere annular mode and an increased duration of weather patterns, resulting in more extreme precipitation events. Under Shared Socioeconomic Pathways SSP585 scenario, extreme precipitation increases by 8.7% along with wave amplitude increase of 7.9° by 2100.
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spelling doaj.art-eeefecc9140d47deac898f957c9745e92023-08-09T15:02:39ZengIOP PublishingEnvironmental Research Letters1748-93262021-01-0116707401210.1088/1748-9326/ac0accProjection of extreme precipitation induced by Arctic amplification over the Northern HemisphereJun Liu0https://orcid.org/0000-0003-1019-3865Dongyou Wu1Xuanye Xu2Mingxia Ji3Quanliang Chen4Xin Wang5Key Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences, Lanzhou University , Lanzhou, People’s Republic of China; School of Earth System Science, Tianjin University , Tianjin, People’s Republic of ChinaKey Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences, Lanzhou University , Lanzhou, People’s Republic of ChinaCollege of Atmospheric Sciences, Chengdu University of Information Technology , Chengdu, People’s Republic of ChinaKey Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences, Lanzhou University , Lanzhou, People’s Republic of ChinaCollege of Atmospheric Sciences, Chengdu University of Information Technology , Chengdu, People’s Republic of ChinaKey Laboratory for Semi-Arid Climate Change of the Ministry of Education, College of Atmospheric Sciences, Lanzhou University , Lanzhou, People’s Republic of China; School of Earth System Science, Tianjin University , Tianjin, People’s Republic of ChinaNumerous attempts have been made to understand the connection between extreme weather and Arctic amplification (AA), and it is still disputed whether the mechanism is the elongation and deceleration of planetary-scale waves. In this study, we provide further evidence that the Arctic’s rapid warming is influencing extreme precipitation in the Northern Hermisphere based on observation and model outputs, and elucidate the underlying dynamic mechanisms. We find that AA has a significant positive correlation with extreme precipitation, both in the past (1901–2018) and in the future (by 2100). Moreover, observations reveal that, with the enhancement of AA since the mid-1980s, the planetary-scale wave amplitude has increased significantly at 0.66°/decade. This is associated with a negative Northern Hemisphere annular mode and an increased duration of weather patterns, resulting in more extreme precipitation events. Under Shared Socioeconomic Pathways SSP585 scenario, extreme precipitation increases by 8.7% along with wave amplitude increase of 7.9° by 2100.https://doi.org/10.1088/1748-9326/ac0accArctic amplificationextreme weatherdynamic mechanismsCMIP6
spellingShingle Jun Liu
Dongyou Wu
Xuanye Xu
Mingxia Ji
Quanliang Chen
Xin Wang
Projection of extreme precipitation induced by Arctic amplification over the Northern Hemisphere
Environmental Research Letters
Arctic amplification
extreme weather
dynamic mechanisms
CMIP6
title Projection of extreme precipitation induced by Arctic amplification over the Northern Hemisphere
title_full Projection of extreme precipitation induced by Arctic amplification over the Northern Hemisphere
title_fullStr Projection of extreme precipitation induced by Arctic amplification over the Northern Hemisphere
title_full_unstemmed Projection of extreme precipitation induced by Arctic amplification over the Northern Hemisphere
title_short Projection of extreme precipitation induced by Arctic amplification over the Northern Hemisphere
title_sort projection of extreme precipitation induced by arctic amplification over the northern hemisphere
topic Arctic amplification
extreme weather
dynamic mechanisms
CMIP6
url https://doi.org/10.1088/1748-9326/ac0acc
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