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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Main Authors: Sarah Feron, Raúl R. Cordero, Alessandro Damiani, Avni Malhotra, Gunther Seckmeyer, Pedro Llanillo
Format: Article
Language:English
Published: Nature Publishing Group 2021-10-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-021-98619-z
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spelling 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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