دورية أكاديمية
Brief communication: Thwaites Glacier cavity evolution
العنوان: | Brief communication: Thwaites Glacier cavity evolution |
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المؤلفون: | S. L. Bevan, A. J. Luckman, D. I. Benn, S. Adusumilli, A. Crawford |
المصدر: | The Cryosphere, Vol 15, Pp 3317-3328 (2021) |
بيانات النشر: | Copernicus Publications, 2021. |
سنة النشر: | 2021 |
المجموعة: | LCC:Environmental sciences LCC:Geology |
مصطلحات موضوعية: | Environmental sciences, GE1-350, Geology, QE1-996.5 |
الوصف: | 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 continued, with an increase in speed of 400 m a−1 and a thinning rate of at least 1.5 m a−1, between 2012 and 2020. |
نوع الوثيقة: | article |
وصف الملف: | electronic resource |
اللغة: | English |
تدمد: | 3317-2021 1994-0416 1994-0424 |
Relation: | https://tc.copernicus.org/articles/15/3317/2021/tc-15-3317-2021.pdf; https://doaj.org/toc/1994-0416; https://doaj.org/toc/1994-0424 |
DOI: | 10.5194/tc-15-3317-2021 |
URL الوصول: | https://doaj.org/article/f6d325f481bd4339ac1cfdcc1d3dd126 |
رقم الأكسشن: | edsdoj.f6d325f481bd4339ac1cfdcc1d3dd126 |
قاعدة البيانات: | Directory of Open Access Journals |
تدمد: | 33172021 19940416 19940424 |
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DOI: | 10.5194/tc-15-3317-2021 |