Impact of a localized source of subglacial discharge on the heat flux and submarine melting of a tidewater glacier: A laboratory study

Idealized laboratory experiments have been conducted in a two-layer stratified fluid to investigate the leading-order dynamics that control submarine melting and meltwater export near a vertical ice-ocean interface as a function of subglacial discharge. In summer, the discharge of surface runoff at...

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Published in:Journal of Physical Oceanography
Main Authors: Cenedese, Claudia (author), Gatto, V.M. (author)
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Online Access:http://resolver.tudelft.nl/uuid:03541777-c963-4471-ab88-79cfaee7a51b
https://doi.org/10.1175/JPO-D-16-0123.1
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spelling fttudelft:oai:tudelft.nl:uuid:03541777-c963-4471-ab88-79cfaee7a51b 2024-04-28T08:40:31+00:00 Impact of a localized source of subglacial discharge on the heat flux and submarine melting of a tidewater glacier: A laboratory study Cenedese, Claudia (author) Gatto, V.M. (author) 2016 http://resolver.tudelft.nl/uuid:03541777-c963-4471-ab88-79cfaee7a51b https://doi.org/10.1175/JPO-D-16-0123.1 en eng http://www.scopus.com/inward/record.url?scp=84994171974&partnerID=8YFLogxK http://resolver.tudelft.nl/uuid:03541777-c963-4471-ab88-79cfaee7a51b Journal of Physical Oceanography--0022-3670--b88f1450-5ec1-4698-8e0c-cb1a1fd3fbce https://doi.org/10.1175/JPO-D-16-0123.1 © 2016 Claudia Cenedese, V.M. Gatto journal article 2016 fttudelft https://doi.org/10.1175/JPO-D-16-0123.1 2024-04-09T23:41:36Z Idealized laboratory experiments have been conducted in a two-layer stratified fluid to investigate the leading-order dynamics that control submarine melting and meltwater export near a vertical ice-ocean interface as a function of subglacial discharge. In summer, the discharge of surface runoff at the base of a glacier (subglacial discharge) generates strong buoyant plumes that rise along the glacier front entraining ambient water along the way. The entrainment enhances the heat transport toward the glacier front and hence the submarine melt rate increases with the subglacial discharge rate. In the laboratory, the effect of subglacial discharge is simulated by introducing freshwater at freezing temperature from a point source at the base ofan ice block representing the glacier. The circulation pattern observed both with and without subglacial discharge resembles those observed in previous observational and numerical studies. Buoyant plumes rise vertically until they find either their neutrally buoyant level or the free surface. Hence, the meltwater can deposit within the interior of the water column and not entirely at the free surface, as confirmed by field observations. The heat budget in the tank, calculated following a new framework, gives estimates of submarine melt rate that increase with the subglacial discharge and are in agreement with the directly measured submarine melting. This laboratory study provides the first direct measurements of submarine melt rates for different subglacial discharges, and the results are consistent with the predictions of previous theoretical and numerical studies. Coastal Engineering Article in Journal/Newspaper Tidewater Delft University of Technology: Institutional Repository Journal of Physical Oceanography 46 10 3155 3163
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collection Delft University of Technology: Institutional Repository
op_collection_id fttudelft
language English
description Idealized laboratory experiments have been conducted in a two-layer stratified fluid to investigate the leading-order dynamics that control submarine melting and meltwater export near a vertical ice-ocean interface as a function of subglacial discharge. In summer, the discharge of surface runoff at the base of a glacier (subglacial discharge) generates strong buoyant plumes that rise along the glacier front entraining ambient water along the way. The entrainment enhances the heat transport toward the glacier front and hence the submarine melt rate increases with the subglacial discharge rate. In the laboratory, the effect of subglacial discharge is simulated by introducing freshwater at freezing temperature from a point source at the base ofan ice block representing the glacier. The circulation pattern observed both with and without subglacial discharge resembles those observed in previous observational and numerical studies. Buoyant plumes rise vertically until they find either their neutrally buoyant level or the free surface. Hence, the meltwater can deposit within the interior of the water column and not entirely at the free surface, as confirmed by field observations. The heat budget in the tank, calculated following a new framework, gives estimates of submarine melt rate that increase with the subglacial discharge and are in agreement with the directly measured submarine melting. This laboratory study provides the first direct measurements of submarine melt rates for different subglacial discharges, and the results are consistent with the predictions of previous theoretical and numerical studies. Coastal Engineering
format Article in Journal/Newspaper
author Cenedese, Claudia (author)
Gatto, V.M. (author)
spellingShingle Cenedese, Claudia (author)
Gatto, V.M. (author)
Impact of a localized source of subglacial discharge on the heat flux and submarine melting of a tidewater glacier: A laboratory study
author_facet Cenedese, Claudia (author)
Gatto, V.M. (author)
author_sort Cenedese, Claudia (author)
title Impact of a localized source of subglacial discharge on the heat flux and submarine melting of a tidewater glacier: A laboratory study
title_short Impact of a localized source of subglacial discharge on the heat flux and submarine melting of a tidewater glacier: A laboratory study
title_full Impact of a localized source of subglacial discharge on the heat flux and submarine melting of a tidewater glacier: A laboratory study
title_fullStr Impact of a localized source of subglacial discharge on the heat flux and submarine melting of a tidewater glacier: A laboratory study
title_full_unstemmed Impact of a localized source of subglacial discharge on the heat flux and submarine melting of a tidewater glacier: A laboratory study
title_sort impact of a localized source of subglacial discharge on the heat flux and submarine melting of a tidewater glacier: a laboratory study
publishDate 2016
url http://resolver.tudelft.nl/uuid:03541777-c963-4471-ab88-79cfaee7a51b
https://doi.org/10.1175/JPO-D-16-0123.1
genre Tidewater
genre_facet Tidewater
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Journal of Physical Oceanography--0022-3670--b88f1450-5ec1-4698-8e0c-cb1a1fd3fbce
https://doi.org/10.1175/JPO-D-16-0123.1
op_rights © 2016 Claudia Cenedese, V.M. Gatto
op_doi https://doi.org/10.1175/JPO-D-16-0123.1
container_title Journal of Physical Oceanography
container_volume 46
container_issue 10
container_start_page 3155
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