West Antarctic surface melt triggered by atmospheric rivers
Recent major melting events in West Antarctica have raised concerns about a potential hydrofracturing and ice shelf instability. These events often share common forcings of surface melt-like anomalous radiative fluxes, turbulent heat fluxes and föhn winds. Using an atmospheric river detection algori...
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Online Access: | http://nora.nerc.ac.uk/id/eprint/525774/ https://www.nature.com/articles/s41561-019-0460-1 |
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ftnerc:oai:nora.nerc.ac.uk:525774 2024-06-02T07:56:03+00:00 West Antarctic surface melt triggered by atmospheric rivers Wille, Jonathan D. Favier, Vincent Dufour, Ambrose Gorodetskaya, Irina V. Turner, John Agosta, Cecile Codron, Francis 2019-10-28 http://nora.nerc.ac.uk/id/eprint/525774/ https://www.nature.com/articles/s41561-019-0460-1 unknown Nature Research Wille, Jonathan D.; Favier, Vincent; Dufour, Ambrose; Gorodetskaya, Irina V.; Turner, John orcid:0000-0002-6111-5122 Agosta, Cecile; Codron, Francis. 2019 West Antarctic surface melt triggered by atmospheric rivers. Nature Geoscience, 12 (11). 911-916. https://doi.org/10.1038/s41561-019-0460-1 <https://doi.org/10.1038/s41561-019-0460-1> Publication - Article PeerReviewed 2019 ftnerc https://doi.org/10.1038/s41561-019-0460-1 2024-05-07T23:32:29Z Recent major melting events in West Antarctica have raised concerns about a potential hydrofracturing and ice shelf instability. These events often share common forcings of surface melt-like anomalous radiative fluxes, turbulent heat fluxes and föhn winds. Using an atmospheric river detection algorithm developed for Antarctica together with surface melt datasets, we produced a climatology of atmospheric river-related surface melting around Antarctica and show that atmospheric rivers are associated with a large percentage of these surface melt events. Despite their rarity (around 12 events per year in West Antarctica), atmospheric rivers are associated with around 40% of the total summer meltwater generated across the Ross Ice Shelf to nearly 100% in the higher elevation Marie Byrd Land and 40–80% of the total winter meltwater generated on the Wilkins, Bach, George IV and Larsen B and C ice shelves. These events were all related to high-pressure blocking ridges that directed anomalous poleward moisture transport towards the continent. Major melt events in the West Antarctic Ice Sheet only occur about a couple times per decade, but a 1–2 °C warming and continued increase in atmospheric river activity could increase the melt frequency with consequences for ice shelf stability. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet Ice Shelf Ice Shelves Marie Byrd Land Ross Ice Shelf West Antarctica Natural Environment Research Council: NERC Open Research Archive Antarctic Byrd Marie Byrd Land ENVELOPE(-130.000,-130.000,-78.000,-78.000) Ross Ice Shelf West Antarctic Ice Sheet West Antarctica Wilkins ENVELOPE(59.326,59.326,-67.248,-67.248) Nature Geoscience 12 11 911 916 |
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Natural Environment Research Council: NERC Open Research Archive |
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ftnerc |
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unknown |
description |
Recent major melting events in West Antarctica have raised concerns about a potential hydrofracturing and ice shelf instability. These events often share common forcings of surface melt-like anomalous radiative fluxes, turbulent heat fluxes and föhn winds. Using an atmospheric river detection algorithm developed for Antarctica together with surface melt datasets, we produced a climatology of atmospheric river-related surface melting around Antarctica and show that atmospheric rivers are associated with a large percentage of these surface melt events. Despite their rarity (around 12 events per year in West Antarctica), atmospheric rivers are associated with around 40% of the total summer meltwater generated across the Ross Ice Shelf to nearly 100% in the higher elevation Marie Byrd Land and 40–80% of the total winter meltwater generated on the Wilkins, Bach, George IV and Larsen B and C ice shelves. These events were all related to high-pressure blocking ridges that directed anomalous poleward moisture transport towards the continent. Major melt events in the West Antarctic Ice Sheet only occur about a couple times per decade, but a 1–2 °C warming and continued increase in atmospheric river activity could increase the melt frequency with consequences for ice shelf stability. |
format |
Article in Journal/Newspaper |
author |
Wille, Jonathan D. Favier, Vincent Dufour, Ambrose Gorodetskaya, Irina V. Turner, John Agosta, Cecile Codron, Francis |
spellingShingle |
Wille, Jonathan D. Favier, Vincent Dufour, Ambrose Gorodetskaya, Irina V. Turner, John Agosta, Cecile Codron, Francis West Antarctic surface melt triggered by atmospheric rivers |
author_facet |
Wille, Jonathan D. Favier, Vincent Dufour, Ambrose Gorodetskaya, Irina V. Turner, John Agosta, Cecile Codron, Francis |
author_sort |
Wille, Jonathan D. |
title |
West Antarctic surface melt triggered by atmospheric rivers |
title_short |
West Antarctic surface melt triggered by atmospheric rivers |
title_full |
West Antarctic surface melt triggered by atmospheric rivers |
title_fullStr |
West Antarctic surface melt triggered by atmospheric rivers |
title_full_unstemmed |
West Antarctic surface melt triggered by atmospheric rivers |
title_sort |
west antarctic surface melt triggered by atmospheric rivers |
publisher |
Nature Research |
publishDate |
2019 |
url |
http://nora.nerc.ac.uk/id/eprint/525774/ https://www.nature.com/articles/s41561-019-0460-1 |
long_lat |
ENVELOPE(-130.000,-130.000,-78.000,-78.000) ENVELOPE(59.326,59.326,-67.248,-67.248) |
geographic |
Antarctic Byrd Marie Byrd Land Ross Ice Shelf West Antarctic Ice Sheet West Antarctica Wilkins |
geographic_facet |
Antarctic Byrd Marie Byrd Land Ross Ice Shelf West Antarctic Ice Sheet West Antarctica Wilkins |
genre |
Antarc* Antarctic Antarctica Ice Sheet Ice Shelf Ice Shelves Marie Byrd Land Ross Ice Shelf West Antarctica |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet Ice Shelf Ice Shelves Marie Byrd Land Ross Ice Shelf West Antarctica |
op_relation |
Wille, Jonathan D.; Favier, Vincent; Dufour, Ambrose; Gorodetskaya, Irina V.; Turner, John orcid:0000-0002-6111-5122 Agosta, Cecile; Codron, Francis. 2019 West Antarctic surface melt triggered by atmospheric rivers. Nature Geoscience, 12 (11). 911-916. https://doi.org/10.1038/s41561-019-0460-1 <https://doi.org/10.1038/s41561-019-0460-1> |
op_doi |
https://doi.org/10.1038/s41561-019-0460-1 |
container_title |
Nature Geoscience |
container_volume |
12 |
container_issue |
11 |
container_start_page |
911 |
op_container_end_page |
916 |
_version_ |
1800753024116719616 |