The influence of föhn winds on annual and seasonal surface melt on the Larsen C Ice Shelf, Antarctica

Warm, dry föhn winds are observed over the Larsen C Ice Shelf year-round and are thought to contribute to the continuing weakening and collapse of ice shelves on the eastern Antarctic Peninsula (AP). We use a surface energy balance (SEB) model, driven by observations from two locations on the Larsen...

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Published in:The Cryosphere
Main Authors: Turton, Jenny V., Kirchgaessner, Amélie, Ross, Andrew N., King, John C., Kuipers Munneke, Peter
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2020
Subjects:
Online Access:https://doi.org/10.5194/tc-14-4165-2020
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spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00054751 2024-09-09T19:02:52+00:00 The influence of föhn winds on annual and seasonal surface melt on the Larsen C Ice Shelf, Antarctica Turton, Jenny V. Kirchgaessner, Amélie Ross, Andrew N. King, John C. Kuipers Munneke, Peter 2020-11 electronic https://doi.org/10.5194/tc-14-4165-2020 https://noa.gwlb.de/receive/cop_mods_00054751 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00054402/tc-14-4165-2020.pdf https://tc.copernicus.org/articles/14/4165/2020/tc-14-4165-2020.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-14-4165-2020 https://noa.gwlb.de/receive/cop_mods_00054751 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00054402/tc-14-4165-2020.pdf https://tc.copernicus.org/articles/14/4165/2020/tc-14-4165-2020.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2020 ftnonlinearchiv https://doi.org/10.5194/tc-14-4165-2020 2024-06-26T04:43:09Z Warm, dry föhn winds are observed over the Larsen C Ice Shelf year-round and are thought to contribute to the continuing weakening and collapse of ice shelves on the eastern Antarctic Peninsula (AP). We use a surface energy balance (SEB) model, driven by observations from two locations on the Larsen C Ice Shelf and one on the remnants of Larsen B, in combination with output from the Antarctic Mesoscale Prediction System (AMPS), to investigate the year-round impact of föhn winds on the SEB and melt from 2009 to 2012. Föhn winds have an impact on the individual components of the surface energy balance in all seasons and lead to an increase in surface melt in spring, summer and autumn up to 100 km away from the foot of the AP. When föhn winds occur in spring they increase surface melt, extend the melt season and increase the number of melt days within a year. Whilst AMPS is able to simulate the percentage of melt days associated with föhn with high skill, it overestimates the total amount of melting during föhn events and non-föhn events. This study extends previous attempts to quantify the impact of föhn on the Larsen C Ice Shelf by including a 4-year study period and a wider area of interest and provides evidence for föhn-related melting on both the Larsen C and Larsen B ice shelves. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica Ice Shelf Ice Shelves The Cryosphere Niedersächsisches Online-Archiv NOA Antarctic The Antarctic Antarctic Peninsula The Cryosphere 14 11 4165 4180
institution Open Polar
collection Niedersächsisches Online-Archiv NOA
op_collection_id ftnonlinearchiv
language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Turton, Jenny V.
Kirchgaessner, Amélie
Ross, Andrew N.
King, John C.
Kuipers Munneke, Peter
The influence of föhn winds on annual and seasonal surface melt on the Larsen C Ice Shelf, Antarctica
topic_facet article
Verlagsveröffentlichung
description Warm, dry föhn winds are observed over the Larsen C Ice Shelf year-round and are thought to contribute to the continuing weakening and collapse of ice shelves on the eastern Antarctic Peninsula (AP). We use a surface energy balance (SEB) model, driven by observations from two locations on the Larsen C Ice Shelf and one on the remnants of Larsen B, in combination with output from the Antarctic Mesoscale Prediction System (AMPS), to investigate the year-round impact of föhn winds on the SEB and melt from 2009 to 2012. Föhn winds have an impact on the individual components of the surface energy balance in all seasons and lead to an increase in surface melt in spring, summer and autumn up to 100 km away from the foot of the AP. When föhn winds occur in spring they increase surface melt, extend the melt season and increase the number of melt days within a year. Whilst AMPS is able to simulate the percentage of melt days associated with föhn with high skill, it overestimates the total amount of melting during föhn events and non-föhn events. This study extends previous attempts to quantify the impact of föhn on the Larsen C Ice Shelf by including a 4-year study period and a wider area of interest and provides evidence for föhn-related melting on both the Larsen C and Larsen B ice shelves.
format Article in Journal/Newspaper
author Turton, Jenny V.
Kirchgaessner, Amélie
Ross, Andrew N.
King, John C.
Kuipers Munneke, Peter
author_facet Turton, Jenny V.
Kirchgaessner, Amélie
Ross, Andrew N.
King, John C.
Kuipers Munneke, Peter
author_sort Turton, Jenny V.
title The influence of föhn winds on annual and seasonal surface melt on the Larsen C Ice Shelf, Antarctica
title_short The influence of föhn winds on annual and seasonal surface melt on the Larsen C Ice Shelf, Antarctica
title_full The influence of föhn winds on annual and seasonal surface melt on the Larsen C Ice Shelf, Antarctica
title_fullStr The influence of föhn winds on annual and seasonal surface melt on the Larsen C Ice Shelf, Antarctica
title_full_unstemmed The influence of föhn winds on annual and seasonal surface melt on the Larsen C Ice Shelf, Antarctica
title_sort influence of föhn winds on annual and seasonal surface melt on the larsen c ice shelf, antarctica
publisher Copernicus Publications
publishDate 2020
url https://doi.org/10.5194/tc-14-4165-2020
https://noa.gwlb.de/receive/cop_mods_00054751
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00054402/tc-14-4165-2020.pdf
https://tc.copernicus.org/articles/14/4165/2020/tc-14-4165-2020.pdf
geographic Antarctic
The Antarctic
Antarctic Peninsula
geographic_facet Antarctic
The Antarctic
Antarctic Peninsula
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Ice Shelf
Ice Shelves
The Cryosphere
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Ice Shelf
Ice Shelves
The Cryosphere
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-14-4165-2020
https://noa.gwlb.de/receive/cop_mods_00054751
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00054402/tc-14-4165-2020.pdf
https://tc.copernicus.org/articles/14/4165/2020/tc-14-4165-2020.pdf
op_rights https://creativecommons.org/licenses/by/4.0/
uneingeschränkt
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/tc-14-4165-2020
container_title The Cryosphere
container_volume 14
container_issue 11
container_start_page 4165
op_container_end_page 4180
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