Brief Communication: Thwaites Glacier cavity evolution

Between 2014 and 2017, ocean melt eroded a large cavity beneath and along the western margin of the fast-flowing core of Thwaites Glacier. Here we show that from 2017 to the end of 2020 the cavity persisted but did not expand. This behaviour, of melt concentrated at the grounding line within confine...

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Main Authors: Bevan, Suzanne L., Luckman, Adrian J., Benn, Douglas I., Adusumilli, Susheel, Crawford, Anna
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/tc-2021-66
https://tc.copernicus.org/preprints/tc-2021-66/
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spelling ftcopernicus:oai:publications.copernicus.org:tcd93106 2023-05-15T18:33:01+02:00 Brief Communication: Thwaites Glacier cavity evolution Bevan, Suzanne L. Luckman, Adrian J. Benn, Douglas I. Adusumilli, Susheel Crawford, Anna 2021-03-04 application/pdf https://doi.org/10.5194/tc-2021-66 https://tc.copernicus.org/preprints/tc-2021-66/ eng eng doi:10.5194/tc-2021-66 https://tc.copernicus.org/preprints/tc-2021-66/ eISSN: 1994-0424 Text 2021 ftcopernicus https://doi.org/10.5194/tc-2021-66 2021-03-08T17:22:13Z Between 2014 and 2017, ocean melt eroded a large cavity beneath and along the western margin of the fast-flowing core of Thwaites Glacier. Here we show that from 2017 to the end of 2020 the cavity persisted but did not expand. This behaviour, of melt concentrated at the grounding line within confined sub-shelf cavities, fits with prior observations and modelling studies. We also show that acceleration and thinning of Thwaites Glacier grounded ice continue, with an increase in speed of 400 ma −1 and a thinning rate of 1.5 ma −1 , between 2012 and 2020. Text Thwaites Glacier Copernicus Publications: E-Journals Thwaites Glacier ENVELOPE(-106.750,-106.750,-75.500,-75.500)
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Between 2014 and 2017, ocean melt eroded a large cavity beneath and along the western margin of the fast-flowing core of Thwaites Glacier. Here we show that from 2017 to the end of 2020 the cavity persisted but did not expand. This behaviour, of melt concentrated at the grounding line within confined sub-shelf cavities, fits with prior observations and modelling studies. We also show that acceleration and thinning of Thwaites Glacier grounded ice continue, with an increase in speed of 400 ma −1 and a thinning rate of 1.5 ma −1 , between 2012 and 2020.
format Text
author Bevan, Suzanne L.
Luckman, Adrian J.
Benn, Douglas I.
Adusumilli, Susheel
Crawford, Anna
spellingShingle Bevan, Suzanne L.
Luckman, Adrian J.
Benn, Douglas I.
Adusumilli, Susheel
Crawford, Anna
Brief Communication: Thwaites Glacier cavity evolution
author_facet Bevan, Suzanne L.
Luckman, Adrian J.
Benn, Douglas I.
Adusumilli, Susheel
Crawford, Anna
author_sort Bevan, Suzanne L.
title Brief Communication: Thwaites Glacier cavity evolution
title_short Brief Communication: Thwaites Glacier cavity evolution
title_full Brief Communication: Thwaites Glacier cavity evolution
title_fullStr Brief Communication: Thwaites Glacier cavity evolution
title_full_unstemmed Brief Communication: Thwaites Glacier cavity evolution
title_sort brief communication: thwaites glacier cavity evolution
publishDate 2021
url https://doi.org/10.5194/tc-2021-66
https://tc.copernicus.org/preprints/tc-2021-66/
long_lat ENVELOPE(-106.750,-106.750,-75.500,-75.500)
geographic Thwaites Glacier
geographic_facet Thwaites Glacier
genre Thwaites Glacier
genre_facet Thwaites Glacier
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-2021-66
https://tc.copernicus.org/preprints/tc-2021-66/
op_doi https://doi.org/10.5194/tc-2021-66
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