Modeling the dynamic response of outlet glaciers to observed ice-shelf thinning in the Bellingshausen Sea Sector, West Antarctica

Satellite observations of gravity anomalies, ice-surface elevation and glacier velocity show significant increases in net grounded-ice-mass loss over the past decade along the Bellingshausen Sea sector (BSS), West Antarctica, in areas where warm (>1°C) sea water floods the continental shelf. Thes...

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Published in:Journal of Glaciology
Main Authors: BRENT M. MINCHEW, G. HILMAR GUDMUNDSSON, ALEX S. GARDNER, FERNANDO S. PAOLO, HELEN A. FRICKER
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2018
Subjects:
Online Access:https://doi.org/10.1017/jog.2018.24
https://doaj.org/article/a49c313a77c94603a8523575c03694b6
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spelling ftdoajarticles:oai:doaj.org/article:a49c313a77c94603a8523575c03694b6 2023-05-15T14:13:29+02:00 Modeling the dynamic response of outlet glaciers to observed ice-shelf thinning in the Bellingshausen Sea Sector, West Antarctica BRENT M. MINCHEW G. HILMAR GUDMUNDSSON ALEX S. GARDNER FERNANDO S. PAOLO HELEN A. FRICKER 2018-04-01T00:00:00Z https://doi.org/10.1017/jog.2018.24 https://doaj.org/article/a49c313a77c94603a8523575c03694b6 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143018000242/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2018.24 0022-1430 1727-5652 https://doaj.org/article/a49c313a77c94603a8523575c03694b6 Journal of Glaciology, Vol 64, Pp 333-342 (2018) glacier flow glacier modeling glaciological model experiments ice–ocean interactions ice shelves Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2018 ftdoajarticles https://doi.org/10.1017/jog.2018.24 2023-03-12T01:30:59Z Satellite observations of gravity anomalies, ice-surface elevation and glacier velocity show significant increases in net grounded-ice-mass loss over the past decade along the Bellingshausen Sea sector (BSS), West Antarctica, in areas where warm (>1°C) sea water floods the continental shelf. These observations provide compelling but indirect evidence that mass losses are driven primarily by reduced buttressing from the floating ice shelves caused by ocean-driven ice-shelf thinning. Here, we combine recent observations of ice velocity, thickness and thickness changes with an ice flow model to study the instantaneous dynamic response of BSS outlet glaciers to observed ice-shelf thinning, alone. Our model results show that multiple BSS outlet glaciers respond instantaneously to observed ice-shelf thinning, particularly in areas where ice shelves ground at discrete points. Increases in modeled and observed dynamic mass losses, however, account for ~5% of the mass loss rates estimated from gravity anomalies and changes in ice-surface elevation, suggesting that variations in surface mass balance may be key to understanding recent BSS mass loss. Our approach isolates the impact of ice-shelf thinning on glacier flow and shows that if ice-shelf thinning continues at or above current rates, total BSS mass loss will increase in the next decade. Article in Journal/Newspaper Antarc* Antarctica Bellingshausen Sea Ice Shelf Ice Shelves Journal of Glaciology West Antarctica Directory of Open Access Journals: DOAJ Articles Bellingshausen Sea West Antarctica Journal of Glaciology 64 244 333 342
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic glacier flow
glacier modeling
glaciological model experiments
ice–ocean interactions
ice shelves
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle glacier flow
glacier modeling
glaciological model experiments
ice–ocean interactions
ice shelves
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
BRENT M. MINCHEW
G. HILMAR GUDMUNDSSON
ALEX S. GARDNER
FERNANDO S. PAOLO
HELEN A. FRICKER
Modeling the dynamic response of outlet glaciers to observed ice-shelf thinning in the Bellingshausen Sea Sector, West Antarctica
topic_facet glacier flow
glacier modeling
glaciological model experiments
ice–ocean interactions
ice shelves
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Satellite observations of gravity anomalies, ice-surface elevation and glacier velocity show significant increases in net grounded-ice-mass loss over the past decade along the Bellingshausen Sea sector (BSS), West Antarctica, in areas where warm (>1°C) sea water floods the continental shelf. These observations provide compelling but indirect evidence that mass losses are driven primarily by reduced buttressing from the floating ice shelves caused by ocean-driven ice-shelf thinning. Here, we combine recent observations of ice velocity, thickness and thickness changes with an ice flow model to study the instantaneous dynamic response of BSS outlet glaciers to observed ice-shelf thinning, alone. Our model results show that multiple BSS outlet glaciers respond instantaneously to observed ice-shelf thinning, particularly in areas where ice shelves ground at discrete points. Increases in modeled and observed dynamic mass losses, however, account for ~5% of the mass loss rates estimated from gravity anomalies and changes in ice-surface elevation, suggesting that variations in surface mass balance may be key to understanding recent BSS mass loss. Our approach isolates the impact of ice-shelf thinning on glacier flow and shows that if ice-shelf thinning continues at or above current rates, total BSS mass loss will increase in the next decade.
format Article in Journal/Newspaper
author BRENT M. MINCHEW
G. HILMAR GUDMUNDSSON
ALEX S. GARDNER
FERNANDO S. PAOLO
HELEN A. FRICKER
author_facet BRENT M. MINCHEW
G. HILMAR GUDMUNDSSON
ALEX S. GARDNER
FERNANDO S. PAOLO
HELEN A. FRICKER
author_sort BRENT M. MINCHEW
title Modeling the dynamic response of outlet glaciers to observed ice-shelf thinning in the Bellingshausen Sea Sector, West Antarctica
title_short Modeling the dynamic response of outlet glaciers to observed ice-shelf thinning in the Bellingshausen Sea Sector, West Antarctica
title_full Modeling the dynamic response of outlet glaciers to observed ice-shelf thinning in the Bellingshausen Sea Sector, West Antarctica
title_fullStr Modeling the dynamic response of outlet glaciers to observed ice-shelf thinning in the Bellingshausen Sea Sector, West Antarctica
title_full_unstemmed Modeling the dynamic response of outlet glaciers to observed ice-shelf thinning in the Bellingshausen Sea Sector, West Antarctica
title_sort modeling the dynamic response of outlet glaciers to observed ice-shelf thinning in the bellingshausen sea sector, west antarctica
publisher Cambridge University Press
publishDate 2018
url https://doi.org/10.1017/jog.2018.24
https://doaj.org/article/a49c313a77c94603a8523575c03694b6
geographic Bellingshausen Sea
West Antarctica
geographic_facet Bellingshausen Sea
West Antarctica
genre Antarc*
Antarctica
Bellingshausen Sea
Ice Shelf
Ice Shelves
Journal of Glaciology
West Antarctica
genre_facet Antarc*
Antarctica
Bellingshausen Sea
Ice Shelf
Ice Shelves
Journal of Glaciology
West Antarctica
op_source Journal of Glaciology, Vol 64, Pp 333-342 (2018)
op_relation https://www.cambridge.org/core/product/identifier/S0022143018000242/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2018.24
0022-1430
1727-5652
https://doaj.org/article/a49c313a77c94603a8523575c03694b6
op_doi https://doi.org/10.1017/jog.2018.24
container_title Journal of Glaciology
container_volume 64
container_issue 244
container_start_page 333
op_container_end_page 342
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