Impact of West Antarctic ice shelf melting on Southern Ocean hydrography

Previous studies show accelerations of West Antarctic glaciers, implying that basal melt rates of these glaciers were previously small and increased in the middle of the 20th century. This enhanced melting is a likely source of the observed Ross Sea (RS) freshening, but its long-term impact on the S...

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Published in:The Cryosphere
Main Authors: Nakayama, Yoshihiro, Timmermann, Ralph, H. Hellmer, Hartmut
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2020
Subjects:
Online Access:https://doi.org/10.5194/tc-14-2205-2020
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spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00052024 2023-05-15T13:54:46+02:00 Impact of West Antarctic ice shelf melting on Southern Ocean hydrography Nakayama, Yoshihiro Timmermann, Ralph H. Hellmer, Hartmut 2020-07 electronic https://doi.org/10.5194/tc-14-2205-2020 https://noa.gwlb.de/receive/cop_mods_00052024 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00051679/tc-14-2205-2020.pdf https://tc.copernicus.org/articles/14/2205/2020/tc-14-2205-2020.pdf eng eng Copernicus Publications The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-14-2205-2020 https://noa.gwlb.de/receive/cop_mods_00052024 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00051679/tc-14-2205-2020.pdf https://tc.copernicus.org/articles/14/2205/2020/tc-14-2205-2020.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess CC-BY article Verlagsveröffentlichung article Text doc-type:article 2020 ftnonlinearchiv https://doi.org/10.5194/tc-14-2205-2020 2022-02-08T22:36:08Z Previous studies show accelerations of West Antarctic glaciers, implying that basal melt rates of these glaciers were previously small and increased in the middle of the 20th century. This enhanced melting is a likely source of the observed Ross Sea (RS) freshening, but its long-term impact on the Southern Ocean hydrography has not been well investigated. Here, we conduct coupled sea ice–ice shelf–ocean simulations with different levels of ice shelf melting from West Antarctic glaciers. Freshening of RS shelf and bottom water is simulated with enhanced West Antarctic ice shelf melting, while no significant changes in shelf water properties are simulated when West Antarctic ice shelf melting is small. We further show that the freshening caused by glacial meltwater from ice shelves in the Amundsen and Bellingshausen seas can propagate further downstream along the East Antarctic coast into the Weddell Sea. The freshening signal propagates onto the RS continental shelf within a year of model simulation, while it takes roughly 5–10 and 10–15 years to propagate into the region off Cape Darnley and into the Weddell Sea, respectively. This advection of freshening modulates the shelf water properties and possibly impacts the production of Antarctic Bottom Water if the enhanced melting of West Antarctic ice shelves continues for a longer period. Article in Journal/Newspaper Antarc* Antarctic Ice Shelf Ice Shelves Ross Sea Sea ice Southern Ocean The Cryosphere Weddell Sea Niedersächsisches Online-Archiv NOA Antarctic Southern Ocean Weddell Sea Ross Sea Weddell Darnley ENVELOPE(69.717,69.717,-67.717,-67.717) Cape Darnley ENVELOPE(69.567,69.567,-67.738,-67.738) The Cryosphere 14 7 2205 2216
institution Open Polar
collection Niedersächsisches Online-Archiv NOA
op_collection_id ftnonlinearchiv
language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Nakayama, Yoshihiro
Timmermann, Ralph
H. Hellmer, Hartmut
Impact of West Antarctic ice shelf melting on Southern Ocean hydrography
topic_facet article
Verlagsveröffentlichung
description Previous studies show accelerations of West Antarctic glaciers, implying that basal melt rates of these glaciers were previously small and increased in the middle of the 20th century. This enhanced melting is a likely source of the observed Ross Sea (RS) freshening, but its long-term impact on the Southern Ocean hydrography has not been well investigated. Here, we conduct coupled sea ice–ice shelf–ocean simulations with different levels of ice shelf melting from West Antarctic glaciers. Freshening of RS shelf and bottom water is simulated with enhanced West Antarctic ice shelf melting, while no significant changes in shelf water properties are simulated when West Antarctic ice shelf melting is small. We further show that the freshening caused by glacial meltwater from ice shelves in the Amundsen and Bellingshausen seas can propagate further downstream along the East Antarctic coast into the Weddell Sea. The freshening signal propagates onto the RS continental shelf within a year of model simulation, while it takes roughly 5–10 and 10–15 years to propagate into the region off Cape Darnley and into the Weddell Sea, respectively. This advection of freshening modulates the shelf water properties and possibly impacts the production of Antarctic Bottom Water if the enhanced melting of West Antarctic ice shelves continues for a longer period.
format Article in Journal/Newspaper
author Nakayama, Yoshihiro
Timmermann, Ralph
H. Hellmer, Hartmut
author_facet Nakayama, Yoshihiro
Timmermann, Ralph
H. Hellmer, Hartmut
author_sort Nakayama, Yoshihiro
title Impact of West Antarctic ice shelf melting on Southern Ocean hydrography
title_short Impact of West Antarctic ice shelf melting on Southern Ocean hydrography
title_full Impact of West Antarctic ice shelf melting on Southern Ocean hydrography
title_fullStr Impact of West Antarctic ice shelf melting on Southern Ocean hydrography
title_full_unstemmed Impact of West Antarctic ice shelf melting on Southern Ocean hydrography
title_sort impact of west antarctic ice shelf melting on southern ocean hydrography
publisher Copernicus Publications
publishDate 2020
url https://doi.org/10.5194/tc-14-2205-2020
https://noa.gwlb.de/receive/cop_mods_00052024
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00051679/tc-14-2205-2020.pdf
https://tc.copernicus.org/articles/14/2205/2020/tc-14-2205-2020.pdf
long_lat ENVELOPE(69.717,69.717,-67.717,-67.717)
ENVELOPE(69.567,69.567,-67.738,-67.738)
geographic Antarctic
Southern Ocean
Weddell Sea
Ross Sea
Weddell
Darnley
Cape Darnley
geographic_facet Antarctic
Southern Ocean
Weddell Sea
Ross Sea
Weddell
Darnley
Cape Darnley
genre Antarc*
Antarctic
Ice Shelf
Ice Shelves
Ross Sea
Sea ice
Southern Ocean
The Cryosphere
Weddell Sea
genre_facet Antarc*
Antarctic
Ice Shelf
Ice Shelves
Ross Sea
Sea ice
Southern Ocean
The Cryosphere
Weddell Sea
op_relation The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424
https://doi.org/10.5194/tc-14-2205-2020
https://noa.gwlb.de/receive/cop_mods_00052024
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00051679/tc-14-2205-2020.pdf
https://tc.copernicus.org/articles/14/2205/2020/tc-14-2205-2020.pdf
op_rights https://creativecommons.org/licenses/by/4.0/
uneingeschränkt
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.5194/tc-14-2205-2020
container_title The Cryosphere
container_volume 14
container_issue 7
container_start_page 2205
op_container_end_page 2216
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