Modeling Antarctic ice shelf responses to future climate changes and impacts on the ocean
We investigate basal melting of all Antarctic ice shelves by a circumpolar iceshelf-sea ice-ocean coupled model and estimate the total basal melting of 770944 Gt/yrunder present-day climate conditions. We present a comparison of the basal melting withprevious observational and modeling estimates for...
Published in: | Journal of Geophysical Research: Oceans |
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Online Access: | https://doi.org/10.1002/jgrc.20166 http://ecite.utas.edu.au/109275 |
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ftunivtasecite:oai:ecite.utas.edu.au:109275 2023-05-15T14:03:26+02:00 Modeling Antarctic ice shelf responses to future climate changes and impacts on the ocean Kusahara, K Hasumi, H 2013 application/pdf https://doi.org/10.1002/jgrc.20166 http://ecite.utas.edu.au/109275 en eng Wiley-Blackwell Publishing, Inc. http://ecite.utas.edu.au/109275/1/Kusahara_JGR_2013.pdf http://dx.doi.org/10.1002/jgrc.20166 Kusahara, K and Hasumi, H, Modeling Antarctic ice shelf responses to future climate changes and impacts on the ocean, Journal of Geophysical Research: Oceans, 118 pp. 2454-2475. ISSN 2169-9275 (2013) [Refereed Article] http://ecite.utas.edu.au/109275 Earth Sciences Atmospheric Sciences Climate Change Processes Refereed Article PeerReviewed 2013 ftunivtasecite https://doi.org/10.1002/jgrc.20166 2019-12-13T22:10:00Z We investigate basal melting of all Antarctic ice shelves by a circumpolar iceshelf-sea ice-ocean coupled model and estimate the total basal melting of 770944 Gt/yrunder present-day climate conditions. We present a comparison of the basal melting withprevious observational and modeling estimates for each ice shelf. Heat sources for basalmelting are largely different among the ice shelves. Sensitivities of the basal melting tosurface air warming and to enhanced westerly winds over the Antarctic CircumpolarCurrent are investigated from a series of numerical experiments. In this model the totalbasal melting strongly depends on the surface air warming but is hardly affected by thechange of westerly winds. The magnitude of the basal melting response to the warmingvaries widely from one ice shelf to another. The largest response is found at ice shelves inthe Bellingshausen Sea, followed by those in the Eastern Weddell Sea and the Indiansector. These increases of basal melting are caused by increases of Circumpolar DeepWater and/or Antarctic Surface Water into ice shelf cavities. By contrast, basal melting ofice shelves in the Ross and Weddell Seas is insensitive to the surface air warming,because even in the warming experiments there is high sea ice production at the front ofthe ice shelves that keeps the water temperature to the surface freezing point. Weakeningof the thermohaline circulation driven by Antarctic dense water formation under warmingclimate conditions is enhanced by basal melting of ice shelves. Article in Journal/Newspaper Antarc* Antarctic Bellingshausen Sea Ice Shelf Ice Shelves Sea ice Weddell Sea eCite UTAS (University of Tasmania) Antarctic Bellingshausen Sea The Antarctic Weddell Weddell Sea Journal of Geophysical Research: Oceans 118 5 2454 2475 |
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Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Atmospheric Sciences Climate Change Processes |
spellingShingle |
Earth Sciences Atmospheric Sciences Climate Change Processes Kusahara, K Hasumi, H Modeling Antarctic ice shelf responses to future climate changes and impacts on the ocean |
topic_facet |
Earth Sciences Atmospheric Sciences Climate Change Processes |
description |
We investigate basal melting of all Antarctic ice shelves by a circumpolar iceshelf-sea ice-ocean coupled model and estimate the total basal melting of 770944 Gt/yrunder present-day climate conditions. We present a comparison of the basal melting withprevious observational and modeling estimates for each ice shelf. Heat sources for basalmelting are largely different among the ice shelves. Sensitivities of the basal melting tosurface air warming and to enhanced westerly winds over the Antarctic CircumpolarCurrent are investigated from a series of numerical experiments. In this model the totalbasal melting strongly depends on the surface air warming but is hardly affected by thechange of westerly winds. The magnitude of the basal melting response to the warmingvaries widely from one ice shelf to another. The largest response is found at ice shelves inthe Bellingshausen Sea, followed by those in the Eastern Weddell Sea and the Indiansector. These increases of basal melting are caused by increases of Circumpolar DeepWater and/or Antarctic Surface Water into ice shelf cavities. By contrast, basal melting ofice shelves in the Ross and Weddell Seas is insensitive to the surface air warming,because even in the warming experiments there is high sea ice production at the front ofthe ice shelves that keeps the water temperature to the surface freezing point. Weakeningof the thermohaline circulation driven by Antarctic dense water formation under warmingclimate conditions is enhanced by basal melting of ice shelves. |
format |
Article in Journal/Newspaper |
author |
Kusahara, K Hasumi, H |
author_facet |
Kusahara, K Hasumi, H |
author_sort |
Kusahara, K |
title |
Modeling Antarctic ice shelf responses to future climate changes and impacts on the ocean |
title_short |
Modeling Antarctic ice shelf responses to future climate changes and impacts on the ocean |
title_full |
Modeling Antarctic ice shelf responses to future climate changes and impacts on the ocean |
title_fullStr |
Modeling Antarctic ice shelf responses to future climate changes and impacts on the ocean |
title_full_unstemmed |
Modeling Antarctic ice shelf responses to future climate changes and impacts on the ocean |
title_sort |
modeling antarctic ice shelf responses to future climate changes and impacts on the ocean |
publisher |
Wiley-Blackwell Publishing, Inc. |
publishDate |
2013 |
url |
https://doi.org/10.1002/jgrc.20166 http://ecite.utas.edu.au/109275 |
geographic |
Antarctic Bellingshausen Sea The Antarctic Weddell Weddell Sea |
geographic_facet |
Antarctic Bellingshausen Sea The Antarctic Weddell Weddell Sea |
genre |
Antarc* Antarctic Bellingshausen Sea Ice Shelf Ice Shelves Sea ice Weddell Sea |
genre_facet |
Antarc* Antarctic Bellingshausen Sea Ice Shelf Ice Shelves Sea ice Weddell Sea |
op_relation |
http://ecite.utas.edu.au/109275/1/Kusahara_JGR_2013.pdf http://dx.doi.org/10.1002/jgrc.20166 Kusahara, K and Hasumi, H, Modeling Antarctic ice shelf responses to future climate changes and impacts on the ocean, Journal of Geophysical Research: Oceans, 118 pp. 2454-2475. ISSN 2169-9275 (2013) [Refereed Article] http://ecite.utas.edu.au/109275 |
op_doi |
https://doi.org/10.1002/jgrc.20166 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
118 |
container_issue |
5 |
container_start_page |
2454 |
op_container_end_page |
2475 |
_version_ |
1766274087410204672 |