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...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley-Blackwell
2017
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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 |