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spelling ftunivsthongkong:oai:repository.ust.hk:1783.1-109982 2023-05-15T13:40:04+02:00 Atmospheric Dynamics Footprint on the January 2016 Ice Sheet Melting in West Antarctica Hu, Xiaoming Sejas, Sergio A. Cai, Ming Li, Zhenning Yang, Song 2019 http://repository.ust.hk/ir/Record/1783.1-109982 https://doi.org/10.1029/2018GL081374 http://lbdiscover.ust.hk/uresolver?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rfr_id=info:sid/HKUST:SPI&rft.genre=article&rft.issn=0094-8276&rft.volume=v. 46&rft.issue=(5)&rft.date=2019&rft.spage=2829&rft.aulast=Hu&rft.aufirst=X.&rft.atitle=Atmospheric+Dynamics+Footprint+on+the+January+2016+Ice+Sheet+Melting+in+West+Antarctica&rft.title=Geophysical+Research+Letters http://www.scopus.com/record/display.url?eid=2-s2.0-85062975509&origin=inward http://gateway.isiknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=LinksAMR&SrcApp=PARTNER_APP&DestLinkType=FullRecord&DestApp=WOS&KeyUT=000462612900055 English eng http://repository.ust.hk/ir/Record/1783.1-109982 Geophysical Research Letters, v. 46, (5), March 2019, p. 2829-2835 0094-8276 https://doi.org/10.1029/2018GL081374 http://lbdiscover.ust.hk/uresolver?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rfr_id=info:sid/HKUST:SPI&rft.genre=article&rft.issn=0094-8276&rft.volume=v. 46&rft.issue=(5)&rft.date=2019&rft.spage=2829&rft.aulast=Hu&rft.aufirst=X.&rft.atitle=Atmospheric+Dynamics+Footprint+on+the+January+2016+Ice+Sheet+Melting+in+West+Antarctica&rft.title=Geophysical+Research+Letters http://www.scopus.com/record/display.url?eid=2-s2.0-85062975509&origin=inward http://gateway.isiknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=LinksAMR&SrcApp=PARTNER_APP&DestLinkType=FullRecord&DestApp=WOS&KeyUT=000462612900055 Article 2019 ftunivsthongkong https://doi.org/10.1029/2018GL081374 2021-05-07T00:02:47Z In January of 2016, the Ross Sea sector of the West Antarctica ice sheet experienced a 3-week-long melting episode. Here we quantify the association of the large-extent and long-lasting melting event with the enhancement of the downward longwave (LW) radiative fluxes at surface due to water vapor, cloud, and atmospheric dynamic feedbacks using the ERA-Interim data set. The abnormally long-lasting temporal surges of atmospheric moisture, warm air, and low-level clouds increase the downward LW radiative energy flux at the surface during the massive ice-melting period. The concurrent timing and spatial overlap between poleward wind anomalies and positive downward LW radiative surface energy flux anomalies over West Antarctica due to warmer air temperature and increases in atmospheric water vapor and cloud coverage provide direct evidence that warm and moist air advection from lower latitudes to West Antarctica causes the rapid long-lasting warming and vast ice mass loss in January of 2016. ©2019. The Authors. Article in Journal/Newspaper Antarc* Antarctica Ice Sheet Ross Sea West Antarctica The Hong Kong University of Science and Technology: HKUST Institutional Repository Ross Sea West Antarctica Geophysical Research Letters 46 5 2829 2835
institution Open Polar
collection The Hong Kong University of Science and Technology: HKUST Institutional Repository
op_collection_id ftunivsthongkong
language English
description In January of 2016, the Ross Sea sector of the West Antarctica ice sheet experienced a 3-week-long melting episode. Here we quantify the association of the large-extent and long-lasting melting event with the enhancement of the downward longwave (LW) radiative fluxes at surface due to water vapor, cloud, and atmospheric dynamic feedbacks using the ERA-Interim data set. The abnormally long-lasting temporal surges of atmospheric moisture, warm air, and low-level clouds increase the downward LW radiative energy flux at the surface during the massive ice-melting period. The concurrent timing and spatial overlap between poleward wind anomalies and positive downward LW radiative surface energy flux anomalies over West Antarctica due to warmer air temperature and increases in atmospheric water vapor and cloud coverage provide direct evidence that warm and moist air advection from lower latitudes to West Antarctica causes the rapid long-lasting warming and vast ice mass loss in January of 2016. ©2019. The Authors.
format Article in Journal/Newspaper
author Hu, Xiaoming
Sejas, Sergio A.
Cai, Ming
Li, Zhenning
Yang, Song
spellingShingle Hu, Xiaoming
Sejas, Sergio A.
Cai, Ming
Li, Zhenning
Yang, Song
Atmospheric Dynamics Footprint on the January 2016 Ice Sheet Melting in West Antarctica
author_facet Hu, Xiaoming
Sejas, Sergio A.
Cai, Ming
Li, Zhenning
Yang, Song
author_sort Hu, Xiaoming
title Atmospheric Dynamics Footprint on the January 2016 Ice Sheet Melting in West Antarctica
title_short Atmospheric Dynamics Footprint on the January 2016 Ice Sheet Melting in West Antarctica
title_full Atmospheric Dynamics Footprint on the January 2016 Ice Sheet Melting in West Antarctica
title_fullStr Atmospheric Dynamics Footprint on the January 2016 Ice Sheet Melting in West Antarctica
title_full_unstemmed Atmospheric Dynamics Footprint on the January 2016 Ice Sheet Melting in West Antarctica
title_sort atmospheric dynamics footprint on the january 2016 ice sheet melting in west antarctica
publishDate 2019
url http://repository.ust.hk/ir/Record/1783.1-109982
https://doi.org/10.1029/2018GL081374
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geographic Ross Sea
West Antarctica
geographic_facet Ross Sea
West Antarctica
genre Antarc*
Antarctica
Ice Sheet
Ross Sea
West Antarctica
genre_facet Antarc*
Antarctica
Ice Sheet
Ross Sea
West Antarctica
op_relation http://repository.ust.hk/ir/Record/1783.1-109982
Geophysical Research Letters, v. 46, (5), March 2019, p. 2829-2835
0094-8276
https://doi.org/10.1029/2018GL081374
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op_doi https://doi.org/10.1029/2018GL081374
container_title Geophysical Research Letters
container_volume 46
container_issue 5
container_start_page 2829
op_container_end_page 2835
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