Warming events projected to become more frequent and last longer across Antarctica
Abstract Summer temperatures are often above freezing along the Antarctic coastline, which makes ice shelves and coastal snowpacks vulnerable to warming events (understood as periods of consecutive days with warmer than usual conditions). Here, we project changes in the frequency, duration and ampli...
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2021-10-01
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Series: | Scientific Reports |
Online Access: | https://doi.org/10.1038/s41598-021-98619-z |
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doaj-1c0a4ee0f068400bb853c796bc648ae12021-10-03T11:35:29ZengNature Publishing GroupScientific Reports2045-23222021-10-011111910.1038/s41598-021-98619-zWarming events projected to become more frequent and last longer across AntarcticaSarah Feron0Raúl R. Cordero1Alessandro Damiani2Avni Malhotra3Gunther Seckmeyer4Pedro Llanillo5University of GroningenUniversidad de SantiagoCenter for Environmental Remote Sensing, Chiba UniversityUniversity of ZurichLeibniz Universität HannoverAlfred Wegener Institute (AWI)Abstract Summer temperatures are often above freezing along the Antarctic coastline, which makes ice shelves and coastal snowpacks vulnerable to warming events (understood as periods of consecutive days with warmer than usual conditions). Here, we project changes in the frequency, duration and amplitude of summertime warming events expected until end of century according to two emission scenarios. By using both global and regional climate models, we found that these events are expected to be more frequent and last longer, continent-wide. By end of century, the number of warming events is projected to double in most of West Antarctica and to triple in the vast interior of East Antarctica, even under a moderate-emission scenario. We also found that the expected rise of warming events in coastal areas surrounding the continent will likely lead to enhanced surface melt, which may pose a risk for the future stability of several Antarctic ice shelves.https://doi.org/10.1038/s41598-021-98619-z |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Sarah Feron Raúl R. Cordero Alessandro Damiani Avni Malhotra Gunther Seckmeyer Pedro Llanillo |
spellingShingle |
Sarah Feron Raúl R. Cordero Alessandro Damiani Avni Malhotra Gunther Seckmeyer Pedro Llanillo Warming events projected to become more frequent and last longer across Antarctica Scientific Reports |
author_facet |
Sarah Feron Raúl R. Cordero Alessandro Damiani Avni Malhotra Gunther Seckmeyer Pedro Llanillo |
author_sort |
Sarah Feron |
title |
Warming events projected to become more frequent and last longer across Antarctica |
title_short |
Warming events projected to become more frequent and last longer across Antarctica |
title_full |
Warming events projected to become more frequent and last longer across Antarctica |
title_fullStr |
Warming events projected to become more frequent and last longer across Antarctica |
title_full_unstemmed |
Warming events projected to become more frequent and last longer across Antarctica |
title_sort |
warming events projected to become more frequent and last longer across antarctica |
publisher |
Nature Publishing Group |
series |
Scientific Reports |
issn |
2045-2322 |
publishDate |
2021-10-01 |
description |
Abstract Summer temperatures are often above freezing along the Antarctic coastline, which makes ice shelves and coastal snowpacks vulnerable to warming events (understood as periods of consecutive days with warmer than usual conditions). Here, we project changes in the frequency, duration and amplitude of summertime warming events expected until end of century according to two emission scenarios. By using both global and regional climate models, we found that these events are expected to be more frequent and last longer, continent-wide. By end of century, the number of warming events is projected to double in most of West Antarctica and to triple in the vast interior of East Antarctica, even under a moderate-emission scenario. We also found that the expected rise of warming events in coastal areas surrounding the continent will likely lead to enhanced surface melt, which may pose a risk for the future stability of several Antarctic ice shelves. |
url |
https://doi.org/10.1038/s41598-021-98619-z |
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