Impacts of Observed Extreme Antarctic Sea Ice Conditions on the Southern Hemisphere Atmosphere

The Antarctic sea ice has undergone dramatic changes in recent years, with the highest recorded sea ice extent in 2014 and the lowest in 2017. We investigated the impacts of the observed changes in these two extremes of Antarctic sea ice conditions on the atmospheric circulation in the Southern Hemi...

Full description

Bibliographic Details
Published in:Atmosphere
Main Authors: Zhu Zhu, Mirong Song
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Online Access:https://doi.org/10.3390/atmos14010036
id ftmdpi:oai:mdpi.com:/2073-4433/14/1/36/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2073-4433/14/1/36/ 2023-08-20T03:59:36+02:00 Impacts of Observed Extreme Antarctic Sea Ice Conditions on the Southern Hemisphere Atmosphere Zhu Zhu Mirong Song agris 2022-12-24 application/pdf https://doi.org/10.3390/atmos14010036 EN eng Multidisciplinary Digital Publishing Institute Atmospheric Techniques, Instruments, and Modeling https://dx.doi.org/10.3390/atmos14010036 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 14; Issue 1; Pages: 36 model simulations Antarctic sea ice Southern Hemisphere climate Text 2022 ftmdpi https://doi.org/10.3390/atmos14010036 2023-08-01T07:57:46Z The Antarctic sea ice has undergone dramatic changes in recent years, with the highest recorded sea ice extent in 2014 and the lowest in 2017. We investigated the impacts of the observed changes in these two extremes of Antarctic sea ice conditions on the atmospheric circulation in the Southern Hemisphere. We conducted three numerical simulations with different seasonal cycles of Antarctic sea ice forcings using the Community Atmosphere Model Version 5: the maximum sea ice extent in 2014 (ICE_14), the minimum sea ice extent in 2017 (ICE_17), and the average sea ice extent between 1981 and 2010 (ICE_clm, reference simulation). Our results suggest that the atmospheric response in the Southern Hemisphere showed strong seasonal variations and the atmospheric circulation in winter was more sensitive to the decreased Antarctic sea ice in 2017 than the increased sea ice in 2014. In ICE_14, the westerlies over the polar region were enhanced in summer, but there was no significant change in the zonal-averaged wind in winter. In contrast, in ICE_17, there was a clear equatorward shift in the subtropical jet in winter, but no significant change in summer. The temperature responses were limited to the Antarctic coast, where there were changes in the sea ice in ICE_14 and ICE_17. The warming on the coast of the Amundsen Sea in summer led to a slight increase in precipitation in both simulations. Text Amundsen Sea Antarc* Antarctic Sea ice MDPI Open Access Publishing Antarctic The Antarctic Amundsen Sea Atmosphere 14 1 36
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic model simulations
Antarctic sea ice
Southern Hemisphere climate
spellingShingle model simulations
Antarctic sea ice
Southern Hemisphere climate
Zhu Zhu
Mirong Song
Impacts of Observed Extreme Antarctic Sea Ice Conditions on the Southern Hemisphere Atmosphere
topic_facet model simulations
Antarctic sea ice
Southern Hemisphere climate
description The Antarctic sea ice has undergone dramatic changes in recent years, with the highest recorded sea ice extent in 2014 and the lowest in 2017. We investigated the impacts of the observed changes in these two extremes of Antarctic sea ice conditions on the atmospheric circulation in the Southern Hemisphere. We conducted three numerical simulations with different seasonal cycles of Antarctic sea ice forcings using the Community Atmosphere Model Version 5: the maximum sea ice extent in 2014 (ICE_14), the minimum sea ice extent in 2017 (ICE_17), and the average sea ice extent between 1981 and 2010 (ICE_clm, reference simulation). Our results suggest that the atmospheric response in the Southern Hemisphere showed strong seasonal variations and the atmospheric circulation in winter was more sensitive to the decreased Antarctic sea ice in 2017 than the increased sea ice in 2014. In ICE_14, the westerlies over the polar region were enhanced in summer, but there was no significant change in the zonal-averaged wind in winter. In contrast, in ICE_17, there was a clear equatorward shift in the subtropical jet in winter, but no significant change in summer. The temperature responses were limited to the Antarctic coast, where there were changes in the sea ice in ICE_14 and ICE_17. The warming on the coast of the Amundsen Sea in summer led to a slight increase in precipitation in both simulations.
format Text
author Zhu Zhu
Mirong Song
author_facet Zhu Zhu
Mirong Song
author_sort Zhu Zhu
title Impacts of Observed Extreme Antarctic Sea Ice Conditions on the Southern Hemisphere Atmosphere
title_short Impacts of Observed Extreme Antarctic Sea Ice Conditions on the Southern Hemisphere Atmosphere
title_full Impacts of Observed Extreme Antarctic Sea Ice Conditions on the Southern Hemisphere Atmosphere
title_fullStr Impacts of Observed Extreme Antarctic Sea Ice Conditions on the Southern Hemisphere Atmosphere
title_full_unstemmed Impacts of Observed Extreme Antarctic Sea Ice Conditions on the Southern Hemisphere Atmosphere
title_sort impacts of observed extreme antarctic sea ice conditions on the southern hemisphere atmosphere
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/atmos14010036
op_coverage agris
geographic Antarctic
The Antarctic
Amundsen Sea
geographic_facet Antarctic
The Antarctic
Amundsen Sea
genre Amundsen Sea
Antarc*
Antarctic
Sea ice
genre_facet Amundsen Sea
Antarc*
Antarctic
Sea ice
op_source Atmosphere; Volume 14; Issue 1; Pages: 36
op_relation Atmospheric Techniques, Instruments, and Modeling
https://dx.doi.org/10.3390/atmos14010036
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos14010036
container_title Atmosphere
container_volume 14
container_issue 1
container_start_page 36
_version_ 1774713704826273792