The Response of Ice Sheets to Climate Variability

West Antarctic Ice Sheet loss is a significant contributor to sea level rise. While the ice loss is thought to be triggered by fluctuations in oceanic heat at the ice shelf bases, ice sheet response to ocean variability remains poorly understood. Using a synchronously coupled ice-ocean model permitt...

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Published in:Geophysical Research Letters
Main Authors: Snow, Kate, Goldberg, Dan, Holland, Paul, Jordan, Jim, Arthern, Robert, Jenkins, Adrian
Format: Article in Journal/Newspaper
Language:English
Published: Wiley-Blackwell 2017
Subjects:
Online Access:https://nrl.northumbria.ac.uk/id/eprint/33709/
https://doi.org/10.1002/2017GL075745
https://nrl.northumbria.ac.uk/id/eprint/33709/1/Snow_et_al-2017-Geophysical_Research_Letters.pdf
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author Snow, Kate
Goldberg, Dan
Holland, Paul
Jordan, Jim
Arthern, Robert
Jenkins, Adrian
author_facet Snow, Kate
Goldberg, Dan
Holland, Paul
Jordan, Jim
Arthern, Robert
Jenkins, Adrian
author_sort Snow, Kate
collection Northumbria University, Newcastle: Northumbria Research Link (NRL)
container_issue 23
container_start_page 11,878
container_title Geophysical Research Letters
container_volume 44
description West Antarctic Ice Sheet loss is a significant contributor to sea level rise. While the ice loss is thought to be triggered by fluctuations in oceanic heat at the ice shelf bases, ice sheet response to ocean variability remains poorly understood. Using a synchronously coupled ice-ocean model permitting grounding line migration, this study evaluates the response of an ice sheet to periodic variations in ocean forcing. Resulting oscillations in grounded ice volume amplitude is shown to grow as a nonlinear function of ocean forcing period. This implies that slower oscillations in climatic forcing are disproportionately important to ice sheets. The ice shelf residence time offers a critical time scale, above which the ice response amplitude is a linear function of ocean forcing period and below which it is quadratic. These results highlight the sensitivity of West Antarctic ice streams to perturbations in heat fluxes occurring at decadal time scales.
format Article in Journal/Newspaper
genre Antarc*
Antarctic
Ice Sheet
Ice Shelf
genre_facet Antarc*
Antarctic
Ice Sheet
Ice Shelf
geographic Antarctic
West Antarctic Ice Sheet
geographic_facet Antarctic
West Antarctic Ice Sheet
id ftunivnorthumb:oai:nrl.northumbria.ac.uk:33709
institution Open Polar
language English
op_collection_id ftunivnorthumb
op_container_end_page 11,885
op_doi https://doi.org/10.1002/2017GL075745
op_relation https://nrl.northumbria.ac.uk/id/eprint/33709/1/Snow_et_al-2017-Geophysical_Research_Letters.pdf
Snow, Kate, Goldberg, Dan, Holland, Paul, Jordan, Jim, Arthern, Robert and Jenkins, Adrian (2017) The Response of Ice Sheets to Climate Variability. Geophysical Research Letters, 44 (23). 11,878-11,885. ISSN 0094-8276
publishDate 2017
publisher Wiley-Blackwell
record_format openpolar
spelling ftunivnorthumb:oai:nrl.northumbria.ac.uk:33709 2025-01-16T19:21:45+00:00 The Response of Ice Sheets to Climate Variability Snow, Kate Goldberg, Dan Holland, Paul Jordan, Jim Arthern, Robert Jenkins, Adrian 2017-12-16 text https://nrl.northumbria.ac.uk/id/eprint/33709/ https://doi.org/10.1002/2017GL075745 https://nrl.northumbria.ac.uk/id/eprint/33709/1/Snow_et_al-2017-Geophysical_Research_Letters.pdf en eng Wiley-Blackwell https://nrl.northumbria.ac.uk/id/eprint/33709/1/Snow_et_al-2017-Geophysical_Research_Letters.pdf Snow, Kate, Goldberg, Dan, Holland, Paul, Jordan, Jim, Arthern, Robert and Jenkins, Adrian (2017) The Response of Ice Sheets to Climate Variability. Geophysical Research Letters, 44 (23). 11,878-11,885. ISSN 0094-8276 F800 Physical and Terrestrial Geographical and Environmental Sciences Article PeerReviewed 2017 ftunivnorthumb https://doi.org/10.1002/2017GL075745 2022-09-25T06:06:57Z West Antarctic Ice Sheet loss is a significant contributor to sea level rise. While the ice loss is thought to be triggered by fluctuations in oceanic heat at the ice shelf bases, ice sheet response to ocean variability remains poorly understood. Using a synchronously coupled ice-ocean model permitting grounding line migration, this study evaluates the response of an ice sheet to periodic variations in ocean forcing. Resulting oscillations in grounded ice volume amplitude is shown to grow as a nonlinear function of ocean forcing period. This implies that slower oscillations in climatic forcing are disproportionately important to ice sheets. The ice shelf residence time offers a critical time scale, above which the ice response amplitude is a linear function of ocean forcing period and below which it is quadratic. These results highlight the sensitivity of West Antarctic ice streams to perturbations in heat fluxes occurring at decadal time scales. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Ice Shelf Northumbria University, Newcastle: Northumbria Research Link (NRL) Antarctic West Antarctic Ice Sheet Geophysical Research Letters 44 23 11,878 11,885
spellingShingle F800 Physical and Terrestrial Geographical and Environmental Sciences
Snow, Kate
Goldberg, Dan
Holland, Paul
Jordan, Jim
Arthern, Robert
Jenkins, Adrian
The Response of Ice Sheets to Climate Variability
title The Response of Ice Sheets to Climate Variability
title_full The Response of Ice Sheets to Climate Variability
title_fullStr The Response of Ice Sheets to Climate Variability
title_full_unstemmed The Response of Ice Sheets to Climate Variability
title_short The Response of Ice Sheets to Climate Variability
title_sort response of ice sheets to climate variability
topic F800 Physical and Terrestrial Geographical and Environmental Sciences
topic_facet F800 Physical and Terrestrial Geographical and Environmental Sciences
url https://nrl.northumbria.ac.uk/id/eprint/33709/
https://doi.org/10.1002/2017GL075745
https://nrl.northumbria.ac.uk/id/eprint/33709/1/Snow_et_al-2017-Geophysical_Research_Letters.pdf