Enhanced Asian warming increases Arctic amplification

The Arctic has been experiencing prominent warming amplification. However, despite anthropogenic emissions and oceanic variability, whether Arctic amplification has a connection with land in the lower latitudes remains unknown. Here, we newly identify enhanced Asian warming as a factor underlying Ar...

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Main Authors: Yongkun Xie, Jianping Huang, Guoxiong Wu, Nan Lei, Yimin Liu
Format: Article
Language:English
Published: IOP Publishing 2023-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/acbdb1
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author Yongkun Xie
Jianping Huang
Guoxiong Wu
Nan Lei
Yimin Liu
author_facet Yongkun Xie
Jianping Huang
Guoxiong Wu
Nan Lei
Yimin Liu
author_sort Yongkun Xie
collection DOAJ
description The Arctic has been experiencing prominent warming amplification. However, despite anthropogenic emissions and oceanic variability, whether Arctic amplification has a connection with land in the lower latitudes remains unknown. Here, we newly identify enhanced Asian warming as a factor underlying Arctic amplification. The simulations demonstrate that enhanced Asian warming contributes 22% of the wintertime amplified warming over the Barents–Kara Seas (BKS). We demonstrate that Asian warming remotely affects the Arctic by affecting poleward atmospheric heat and moisture transport. The external anomalous heat and moisture further trigger local feedbacks concerning sea ice-albedo feedback and changes in longwave radiation and evaporation, thus facilitating BKS warming amplification. The capacitor effect of the Arctic Ocean further modulates the seasonality of BKS warming via turbulent heat flux exchange between the atmosphere and ocean. Moreover, anomalous Rossby wave trains are responsible for the anomalous atmospheric circulations favoring the atmospheric heat and moisture transport into BKS. Our findings illuminate a new factor from remote lower latitudes affecting Arctic climate change.
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spelling doaj.art-d39d7d9424d1470798c9eec694be1c3f2023-08-09T15:13:51ZengIOP PublishingEnvironmental Research Letters1748-93262023-01-0118303404110.1088/1748-9326/acbdb1Enhanced Asian warming increases Arctic amplificationYongkun Xie0Jianping Huang1https://orcid.org/0000-0003-2845-797XGuoxiong Wu2Nan Lei3Yimin Liu4Collaborative Innovation Center for Western Ecological Safety, Lanzhou University , Lanzhou, People’s Republic of ChinaCollaborative Innovation Center for Western Ecological Safety, Lanzhou University , Lanzhou, People’s Republic of ChinaState Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of Sciences , Beijing, People’s Republic of China; College of Earth and Planetary Sciences, University of Chinese Academy of Sciences , Beijing, People’s Republic of ChinaCollaborative Innovation Center for Western Ecological Safety, Lanzhou University , Lanzhou, People’s Republic of China; College of Atmospheric Sciences, Lanzhou University , Lanzhou, People’s Republic of ChinaState Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of Sciences , Beijing, People’s Republic of China; College of Earth and Planetary Sciences, University of Chinese Academy of Sciences , Beijing, People’s Republic of ChinaThe Arctic has been experiencing prominent warming amplification. However, despite anthropogenic emissions and oceanic variability, whether Arctic amplification has a connection with land in the lower latitudes remains unknown. Here, we newly identify enhanced Asian warming as a factor underlying Arctic amplification. The simulations demonstrate that enhanced Asian warming contributes 22% of the wintertime amplified warming over the Barents–Kara Seas (BKS). We demonstrate that Asian warming remotely affects the Arctic by affecting poleward atmospheric heat and moisture transport. The external anomalous heat and moisture further trigger local feedbacks concerning sea ice-albedo feedback and changes in longwave radiation and evaporation, thus facilitating BKS warming amplification. The capacitor effect of the Arctic Ocean further modulates the seasonality of BKS warming via turbulent heat flux exchange between the atmosphere and ocean. Moreover, anomalous Rossby wave trains are responsible for the anomalous atmospheric circulations favoring the atmospheric heat and moisture transport into BKS. Our findings illuminate a new factor from remote lower latitudes affecting Arctic climate change.https://doi.org/10.1088/1748-9326/acbdb1Asian warmingArctic amplificationTibetan PlateaudrylandBarents–Kara Seas
spellingShingle Yongkun Xie
Jianping Huang
Guoxiong Wu
Nan Lei
Yimin Liu
Enhanced Asian warming increases Arctic amplification
Environmental Research Letters
Asian warming
Arctic amplification
Tibetan Plateau
dryland
Barents–Kara Seas
title Enhanced Asian warming increases Arctic amplification
title_full Enhanced Asian warming increases Arctic amplification
title_fullStr Enhanced Asian warming increases Arctic amplification
title_full_unstemmed Enhanced Asian warming increases Arctic amplification
title_short Enhanced Asian warming increases Arctic amplification
title_sort enhanced asian warming increases arctic amplification
topic Asian warming
Arctic amplification
Tibetan Plateau
dryland
Barents–Kara Seas
url https://doi.org/10.1088/1748-9326/acbdb1
work_keys_str_mv AT yongkunxie enhancedasianwarmingincreasesarcticamplification
AT jianpinghuang enhancedasianwarmingincreasesarcticamplification
AT guoxiongwu enhancedasianwarmingincreasesarcticamplification
AT nanlei enhancedasianwarmingincreasesarcticamplification
AT yiminliu enhancedasianwarmingincreasesarcticamplification