Melting temperature changes during slip across subglacial cavities drive basal mass exchange

The importance of glacier sliding has motivated a rich literature describing the thermomechanical interactions between ice, liquid water and bed materials. Early recognition of the gradient in melting temperature across small bed obstacles led to focused studies of regelation. An appreciation for th...

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Main Authors: Alan W. Rempel, Colin R. Meyer, Kiya L. Riverman
Format: Article
Language:English
Published: Cambridge University Press 2022-02-01
Series:Journal of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0022143021001076/type/journal_article
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author Alan W. Rempel
Colin R. Meyer
Kiya L. Riverman
author_facet Alan W. Rempel
Colin R. Meyer
Kiya L. Riverman
author_sort Alan W. Rempel
collection DOAJ
description The importance of glacier sliding has motivated a rich literature describing the thermomechanical interactions between ice, liquid water and bed materials. Early recognition of the gradient in melting temperature across small bed obstacles led to focused studies of regelation. An appreciation for the limits on ice deformation rates downstream of larger obstacles highlighted a role for cavitation, which has subsequently gained prominence in descriptions of subglacial drainage. Here, we show that the changes in melting temperature that accompany changes in normal stress along a sliding ice interface near cavities and other macroscopic drainage elements cause appreciable supercooling and basal mass exchange. This provides the basis of a novel formation mechanism for widely observed laminated debris-rich basal ice layers.
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spelling doaj.art-0c58b305d42142138edf1402c97d88212023-03-09T12:41:13ZengCambridge University PressJournal of Glaciology0022-14301727-56522022-02-016819720310.1017/jog.2021.107Melting temperature changes during slip across subglacial cavities drive basal mass exchangeAlan W. Rempel0Colin R. Meyer1https://orcid.org/0000-0002-1209-1881Kiya L. Riverman2https://orcid.org/0000-0002-8033-3096Department of Earth Sciences, University of Oregon, Eugene OR, USAThayer School of Engineering, Dartmouth College, Hanover NH, USACollege of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis OR, USAThe importance of glacier sliding has motivated a rich literature describing the thermomechanical interactions between ice, liquid water and bed materials. Early recognition of the gradient in melting temperature across small bed obstacles led to focused studies of regelation. An appreciation for the limits on ice deformation rates downstream of larger obstacles highlighted a role for cavitation, which has subsequently gained prominence in descriptions of subglacial drainage. Here, we show that the changes in melting temperature that accompany changes in normal stress along a sliding ice interface near cavities and other macroscopic drainage elements cause appreciable supercooling and basal mass exchange. This provides the basis of a novel formation mechanism for widely observed laminated debris-rich basal ice layers.https://www.cambridge.org/core/product/identifier/S0022143021001076/type/journal_articleBasal iceice physicsmelt-basalsubglacial processes
spellingShingle Alan W. Rempel
Colin R. Meyer
Kiya L. Riverman
Melting temperature changes during slip across subglacial cavities drive basal mass exchange
Journal of Glaciology
Basal ice
ice physics
melt-basal
subglacial processes
title Melting temperature changes during slip across subglacial cavities drive basal mass exchange
title_full Melting temperature changes during slip across subglacial cavities drive basal mass exchange
title_fullStr Melting temperature changes during slip across subglacial cavities drive basal mass exchange
title_full_unstemmed Melting temperature changes during slip across subglacial cavities drive basal mass exchange
title_short Melting temperature changes during slip across subglacial cavities drive basal mass exchange
title_sort melting temperature changes during slip across subglacial cavities drive basal mass exchange
topic Basal ice
ice physics
melt-basal
subglacial processes
url https://www.cambridge.org/core/product/identifier/S0022143021001076/type/journal_article
work_keys_str_mv AT alanwrempel meltingtemperaturechangesduringslipacrosssubglacialcavitiesdrivebasalmassexchange
AT colinrmeyer meltingtemperaturechangesduringslipacrosssubglacialcavitiesdrivebasalmassexchange
AT kiyalriverman meltingtemperaturechangesduringslipacrosssubglacialcavitiesdrivebasalmassexchange