Sensitivity of tidewater glaciers to submarine melting governed by plume locations

The response of tidewater glaciers to ocean warming remains a key uncertainty in sea level rise predictions. Here we use a 3‐D numerical model to examine the response of an idealized tidewater glacier to spatial variations in submarine melt rate. While melting toward the center of the terminus cause...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Cowton, Tom, Todd, Joe A., Benn, Douglas I.
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:https://risweb.st-andrews.ac.uk/portal/en/researchoutput/sensitivity-of-tidewater-glaciers-to-submarine-melting-governed-by-plume-locations(06e3be5f-7854-4747-9d3a-4f866fd004ff).html
https://doi.org/10.1029/2019GL084215
https://research-repository.st-andrews.ac.uk/bitstream/10023/19859/1/Cowton_2019_GRL_Tidewaterglaciers_FinalPubVersion.pdf
id ftunstandrewcris:oai:risweb.st-andrews.ac.uk:publications/06e3be5f-7854-4747-9d3a-4f866fd004ff
record_format openpolar
spelling ftunstandrewcris:oai:risweb.st-andrews.ac.uk:publications/06e3be5f-7854-4747-9d3a-4f866fd004ff 2023-05-15T18:33:03+02:00 Sensitivity of tidewater glaciers to submarine melting governed by plume locations Cowton, Tom Todd, Joe A. Benn, Douglas I. 2019-11-19 application/pdf https://risweb.st-andrews.ac.uk/portal/en/researchoutput/sensitivity-of-tidewater-glaciers-to-submarine-melting-governed-by-plume-locations(06e3be5f-7854-4747-9d3a-4f866fd004ff).html https://doi.org/10.1029/2019GL084215 https://research-repository.st-andrews.ac.uk/bitstream/10023/19859/1/Cowton_2019_GRL_Tidewaterglaciers_FinalPubVersion.pdf eng eng info:eu-repo/semantics/openAccess Cowton , T , Todd , J A & Benn , D I 2019 , ' Sensitivity of tidewater glaciers to submarine melting governed by plume locations ' , Geophysical Research Letters , vol. 46 , no. 20 , pp. 11219-11227 . https://doi.org/10.1029/2019GL084215 Glaciers Ice sheets Calving Submarine melting article 2019 ftunstandrewcris https://doi.org/10.1029/2019GL084215 2021-12-26T14:35:12Z The response of tidewater glaciers to ocean warming remains a key uncertainty in sea level rise predictions. Here we use a 3‐D numerical model to examine the response of an idealized tidewater glacier to spatial variations in submarine melt rate. While melting toward the center of the terminus causes only a localized increase in mass loss, melting near the lateral margins triggers increased calving across the width of the glacier, causing the terminus to retreat at several times the width‐averaged melt rate. This occurs because melting near the margins has a greater disruptive impact on the compressive stress arch that transfers resistance from the side walls to the body of the glacier. We suggest that the rate of terminus advance or retreat may thus be governed by the difference between ice velocity and submarine melting in the slow‐flowing zones away from the glacier center. Article in Journal/Newspaper Tidewater University of St Andrews: Research Portal Geophysical Research Letters 46 20 11219 11227
institution Open Polar
collection University of St Andrews: Research Portal
op_collection_id ftunstandrewcris
language English
topic Glaciers
Ice sheets
Calving
Submarine melting
spellingShingle Glaciers
Ice sheets
Calving
Submarine melting
Cowton, Tom
Todd, Joe A.
Benn, Douglas I.
Sensitivity of tidewater glaciers to submarine melting governed by plume locations
topic_facet Glaciers
Ice sheets
Calving
Submarine melting
description The response of tidewater glaciers to ocean warming remains a key uncertainty in sea level rise predictions. Here we use a 3‐D numerical model to examine the response of an idealized tidewater glacier to spatial variations in submarine melt rate. While melting toward the center of the terminus causes only a localized increase in mass loss, melting near the lateral margins triggers increased calving across the width of the glacier, causing the terminus to retreat at several times the width‐averaged melt rate. This occurs because melting near the margins has a greater disruptive impact on the compressive stress arch that transfers resistance from the side walls to the body of the glacier. We suggest that the rate of terminus advance or retreat may thus be governed by the difference between ice velocity and submarine melting in the slow‐flowing zones away from the glacier center.
format Article in Journal/Newspaper
author Cowton, Tom
Todd, Joe A.
Benn, Douglas I.
author_facet Cowton, Tom
Todd, Joe A.
Benn, Douglas I.
author_sort Cowton, Tom
title Sensitivity of tidewater glaciers to submarine melting governed by plume locations
title_short Sensitivity of tidewater glaciers to submarine melting governed by plume locations
title_full Sensitivity of tidewater glaciers to submarine melting governed by plume locations
title_fullStr Sensitivity of tidewater glaciers to submarine melting governed by plume locations
title_full_unstemmed Sensitivity of tidewater glaciers to submarine melting governed by plume locations
title_sort sensitivity of tidewater glaciers to submarine melting governed by plume locations
publishDate 2019
url https://risweb.st-andrews.ac.uk/portal/en/researchoutput/sensitivity-of-tidewater-glaciers-to-submarine-melting-governed-by-plume-locations(06e3be5f-7854-4747-9d3a-4f866fd004ff).html
https://doi.org/10.1029/2019GL084215
https://research-repository.st-andrews.ac.uk/bitstream/10023/19859/1/Cowton_2019_GRL_Tidewaterglaciers_FinalPubVersion.pdf
genre Tidewater
genre_facet Tidewater
op_source Cowton , T , Todd , J A & Benn , D I 2019 , ' Sensitivity of tidewater glaciers to submarine melting governed by plume locations ' , Geophysical Research Letters , vol. 46 , no. 20 , pp. 11219-11227 . https://doi.org/10.1029/2019GL084215
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1029/2019GL084215
container_title Geophysical Research Letters
container_volume 46
container_issue 20
container_start_page 11219
op_container_end_page 11227
_version_ 1766217342066360320