Subseasonal Reversal of Winter Temperature Over Northeast China in 2014/2015: Role of Arctic Sea Ice

This study investigates the temperature reversal over Northeast China (NEC) in winter 2014/2015, focusing on the variations of related general circulations and the affecting mechanisms of the Arctic sea ice on daily scale. It turns out to be the coupled impacts of the eastward propagations of tropos...

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Published in:Frontiers in Environmental Science
Main Authors: Dai, Haixia, Fan, Ke
Format: Article in Journal/Newspaper
Language:unknown
Published: Frontiers Media SA 2022
Subjects:
Online Access:http://dx.doi.org/10.3389/fenvs.2022.852673
https://www.frontiersin.org/articles/10.3389/fenvs.2022.852673/full
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spelling crfrontiers:10.3389/fenvs.2022.852673 2024-10-13T14:04:49+00:00 Subseasonal Reversal of Winter Temperature Over Northeast China in 2014/2015: Role of Arctic Sea Ice Dai, Haixia Fan, Ke 2022 http://dx.doi.org/10.3389/fenvs.2022.852673 https://www.frontiersin.org/articles/10.3389/fenvs.2022.852673/full unknown Frontiers Media SA https://creativecommons.org/licenses/by/4.0/ Frontiers in Environmental Science volume 10 ISSN 2296-665X journal-article 2022 crfrontiers https://doi.org/10.3389/fenvs.2022.852673 2024-10-01T04:01:09Z This study investigates the temperature reversal over Northeast China (NEC) in winter 2014/2015, focusing on the variations of related general circulations and the affecting mechanisms of the Arctic sea ice on daily scale. It turns out to be the coupled impacts of the eastward propagations of tropospheric wave trains from the North Atlantic Ocean and the downward reflections of planetary wavenumber-1 from the stratosphere that resulted in the subseasonal reversal of winter temperature over NEC in winter 2014/2015. Also, such anomalous atmospheric circulations can be attributed to sea-ice anomalies over the Davis Strait–Baffin Bay (SIC-DSBB) and the Barents–Kara Sea (SIC-BKS) in November 2014. SIC-DSBB anomalies in November 2014 excited the eastward propagation of Rossby waves via the tripole pattern of sea surface temperature over the North Atlantic Sea, leading to the colder condition over NEC in the first and middle 10 days of December 2014. Anomalously heavy SIC-BKS also triggered wave trains from the polar region to Eurasia, strengthening the Rossby wave induced by SIC-DSBB. Moreover, the wave trains suppressed the upward propagation of planetary wavenumber-1 over the Siberia region, strengthening the stratospheric polar vortex. However, the sea-ice anomalies over these two domains only existed in November 2014. Thus, the tropospheric mechanisms by which the Arctic sea ice affected the temperature over NEC only lasted to late December 2014. Meanwhile, the stratospheric anomalies propagated downwards with the planetary wavenumber-1, favoring the positive phase of Arctic Oscillation in the troposphere and the warm condition over NEC since the last week of December 2014. Consequently, the temperature over NEC reversed in winter 2014/2015. Article in Journal/Newspaper Arctic Baffin Bay Baffin Bay Baffin Davis Strait Kara Sea North Atlantic Sea ice Siberia Frontiers (Publisher) Arctic Baffin Bay Kara Sea Frontiers in Environmental Science 10
institution Open Polar
collection Frontiers (Publisher)
op_collection_id crfrontiers
language unknown
description This study investigates the temperature reversal over Northeast China (NEC) in winter 2014/2015, focusing on the variations of related general circulations and the affecting mechanisms of the Arctic sea ice on daily scale. It turns out to be the coupled impacts of the eastward propagations of tropospheric wave trains from the North Atlantic Ocean and the downward reflections of planetary wavenumber-1 from the stratosphere that resulted in the subseasonal reversal of winter temperature over NEC in winter 2014/2015. Also, such anomalous atmospheric circulations can be attributed to sea-ice anomalies over the Davis Strait–Baffin Bay (SIC-DSBB) and the Barents–Kara Sea (SIC-BKS) in November 2014. SIC-DSBB anomalies in November 2014 excited the eastward propagation of Rossby waves via the tripole pattern of sea surface temperature over the North Atlantic Sea, leading to the colder condition over NEC in the first and middle 10 days of December 2014. Anomalously heavy SIC-BKS also triggered wave trains from the polar region to Eurasia, strengthening the Rossby wave induced by SIC-DSBB. Moreover, the wave trains suppressed the upward propagation of planetary wavenumber-1 over the Siberia region, strengthening the stratospheric polar vortex. However, the sea-ice anomalies over these two domains only existed in November 2014. Thus, the tropospheric mechanisms by which the Arctic sea ice affected the temperature over NEC only lasted to late December 2014. Meanwhile, the stratospheric anomalies propagated downwards with the planetary wavenumber-1, favoring the positive phase of Arctic Oscillation in the troposphere and the warm condition over NEC since the last week of December 2014. Consequently, the temperature over NEC reversed in winter 2014/2015.
format Article in Journal/Newspaper
author Dai, Haixia
Fan, Ke
spellingShingle Dai, Haixia
Fan, Ke
Subseasonal Reversal of Winter Temperature Over Northeast China in 2014/2015: Role of Arctic Sea Ice
author_facet Dai, Haixia
Fan, Ke
author_sort Dai, Haixia
title Subseasonal Reversal of Winter Temperature Over Northeast China in 2014/2015: Role of Arctic Sea Ice
title_short Subseasonal Reversal of Winter Temperature Over Northeast China in 2014/2015: Role of Arctic Sea Ice
title_full Subseasonal Reversal of Winter Temperature Over Northeast China in 2014/2015: Role of Arctic Sea Ice
title_fullStr Subseasonal Reversal of Winter Temperature Over Northeast China in 2014/2015: Role of Arctic Sea Ice
title_full_unstemmed Subseasonal Reversal of Winter Temperature Over Northeast China in 2014/2015: Role of Arctic Sea Ice
title_sort subseasonal reversal of winter temperature over northeast china in 2014/2015: role of arctic sea ice
publisher Frontiers Media SA
publishDate 2022
url http://dx.doi.org/10.3389/fenvs.2022.852673
https://www.frontiersin.org/articles/10.3389/fenvs.2022.852673/full
geographic Arctic
Baffin Bay
Kara Sea
geographic_facet Arctic
Baffin Bay
Kara Sea
genre Arctic
Baffin Bay
Baffin Bay
Baffin
Davis Strait
Kara Sea
North Atlantic
Sea ice
Siberia
genre_facet Arctic
Baffin Bay
Baffin Bay
Baffin
Davis Strait
Kara Sea
North Atlantic
Sea ice
Siberia
op_source Frontiers in Environmental Science
volume 10
ISSN 2296-665X
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3389/fenvs.2022.852673
container_title Frontiers in Environmental Science
container_volume 10
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