Modelling the response of ice shelf basal melting to different ocean cavity environmental regimes

We present simulation results from a version of the Regional Ocean Modeling System modified for ice shelf/ocean interaction, including the parameterisation of basal melting by molecular diffusion alone. Simulations investigate the differences in melting for an idealised ice shelf experiencing a rang...

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Main Authors: David E. Gwyther, Eva A. Cougnon, Benjamin K. Galton-Fenzi, Jason L. Roberts, John R. Hunter, Michael S. Dinniman
Format: Article
Language:English
Published: Cambridge University Press 2016-09-01
Series:Annals of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0260305516000318/type/journal_article
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author David E. Gwyther
Eva A. Cougnon
Benjamin K. Galton-Fenzi
Jason L. Roberts
John R. Hunter
Michael S. Dinniman
author_facet David E. Gwyther
Eva A. Cougnon
Benjamin K. Galton-Fenzi
Jason L. Roberts
John R. Hunter
Michael S. Dinniman
author_sort David E. Gwyther
collection DOAJ
description We present simulation results from a version of the Regional Ocean Modeling System modified for ice shelf/ocean interaction, including the parameterisation of basal melting by molecular diffusion alone. Simulations investigate the differences in melting for an idealised ice shelf experiencing a range of cold to hot ocean cavity conditions. Both the pattern of melt and the location of maximum melt shift due to changes in the buoyancy-driven circulation, in a different way to previous studies. Tidal forcing increases both the circulation strength and melting, with the strongest impact on the cold cavity case. Our results highlight the importance of including a complete melt parameterisation and tidal forcing. In response to the 2.4°C ocean warming initially applied to a cold cavity ice shelf, we find that melting will increase by about an order of magnitude (24 × with tides and 41 × without tides).
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spelling doaj.art-7c28ab483f2846c8994ce7c608b25ce72023-03-09T12:27:29ZengCambridge University PressAnnals of Glaciology0260-30551727-56442016-09-015713114110.1017/aog.2016.31Modelling the response of ice shelf basal melting to different ocean cavity environmental regimesDavid E. Gwyther0Eva A. Cougnon1Benjamin K. Galton-Fenzi2Jason L. Roberts3John R. Hunter4Michael S. Dinniman5Institute for Marine and Antarctic Studies, University of Tasmania, Private Bag 129, Hobart, Tasmania 7001, Australia E-mail: Antarctic Climate & Ecosystems Cooperative Research Centre, University of Tasmania, Private Bag 80, Hobart, Tasmania 7001, AustraliaInstitute for Marine and Antarctic Studies, University of Tasmania, Private Bag 129, Hobart, Tasmania 7001, Australia E-mail: Antarctic Climate & Ecosystems Cooperative Research Centre, University of Tasmania, Private Bag 80, Hobart, Tasmania 7001, Australia Commonwealth Scientific and Industrial Research Organisation, Marine and Atmospheric Research, Hobart, AustraliaAntarctic Climate & Ecosystems Cooperative Research Centre, University of Tasmania, Private Bag 80, Hobart, Tasmania 7001, Australia Australian Antarctic Division, Channel Highway, Kingston, Tasmania, 7050, AustraliaAntarctic Climate & Ecosystems Cooperative Research Centre, University of Tasmania, Private Bag 80, Hobart, Tasmania 7001, Australia Australian Antarctic Division, Channel Highway, Kingston, Tasmania, 7050, AustraliaAntarctic Climate & Ecosystems Cooperative Research Centre, University of Tasmania, Private Bag 80, Hobart, Tasmania 7001, AustraliaCenter for Coastal Physical Oceanography, Old Dominion University, Norfolk, VA, USAWe present simulation results from a version of the Regional Ocean Modeling System modified for ice shelf/ocean interaction, including the parameterisation of basal melting by molecular diffusion alone. Simulations investigate the differences in melting for an idealised ice shelf experiencing a range of cold to hot ocean cavity conditions. Both the pattern of melt and the location of maximum melt shift due to changes in the buoyancy-driven circulation, in a different way to previous studies. Tidal forcing increases both the circulation strength and melting, with the strongest impact on the cold cavity case. Our results highlight the importance of including a complete melt parameterisation and tidal forcing. In response to the 2.4°C ocean warming initially applied to a cold cavity ice shelf, we find that melting will increase by about an order of magnitude (24 × with tides and 41 × without tides).https://www.cambridge.org/core/product/identifier/S0260305516000318/type/journal_articleice shelvesice/ocean interactionsmelt - basal
spellingShingle David E. Gwyther
Eva A. Cougnon
Benjamin K. Galton-Fenzi
Jason L. Roberts
John R. Hunter
Michael S. Dinniman
Modelling the response of ice shelf basal melting to different ocean cavity environmental regimes
Annals of Glaciology
ice shelves
ice/ocean interactions
melt - basal
title Modelling the response of ice shelf basal melting to different ocean cavity environmental regimes
title_full Modelling the response of ice shelf basal melting to different ocean cavity environmental regimes
title_fullStr Modelling the response of ice shelf basal melting to different ocean cavity environmental regimes
title_full_unstemmed Modelling the response of ice shelf basal melting to different ocean cavity environmental regimes
title_short Modelling the response of ice shelf basal melting to different ocean cavity environmental regimes
title_sort modelling the response of ice shelf basal melting to different ocean cavity environmental regimes
topic ice shelves
ice/ocean interactions
melt - basal
url https://www.cambridge.org/core/product/identifier/S0260305516000318/type/journal_article
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AT benjaminkgaltonfenzi modellingtheresponseoficeshelfbasalmeltingtodifferentoceancavityenvironmentalregimes
AT jasonlroberts modellingtheresponseoficeshelfbasalmeltingtodifferentoceancavityenvironmentalregimes
AT johnrhunter modellingtheresponseoficeshelfbasalmeltingtodifferentoceancavityenvironmentalregimes
AT michaelsdinniman modellingtheresponseoficeshelfbasalmeltingtodifferentoceancavityenvironmentalregimes