Glacial melt under a porous debris layer
In this paper we undertake a quantitative analysis of the dynamic process by which ice underneath a dry porous debris layer melts. We show that the incorporation of debris-layer airflow into a theoretical model of glacial melting can capture the empirically observed features of the so-called Østrem...
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Language: | English |
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2015
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Online Access: | https://research.manchester.ac.uk/en/publications/f0187075-9c62-4c10-8b3f-0ed497cb3cd5 https://doi.org/10.3189/2015JoG14J235 |
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ftumanchesterpub:oai:pure.atira.dk:publications/f0187075-9c62-4c10-8b3f-0ed497cb3cd5 2023-11-12T04:19:55+01:00 Glacial melt under a porous debris layer Evatt, Geoffrey Abrahams, I David Heil, Matthias Mayer, Christoph Kingslake, Jonathan Mitchell, Sarah L. Fowler, Andrew C. Clark, Christopher D. 2015-11 https://research.manchester.ac.uk/en/publications/f0187075-9c62-4c10-8b3f-0ed497cb3cd5 https://doi.org/10.3189/2015JoG14J235 eng eng info:eu-repo/semantics/closedAccess Evatt , G , Abrahams , I D , Heil , M , Mayer , C , Kingslake , J , Mitchell , S L , Fowler , A C & Clark , C D 2015 , ' Glacial melt under a porous debris layer ' , Journal of Glaciology , vol. 61 , no. 229 , pp. 825-836 . https://doi.org/10.3189/2015JoG14J235 DEBRIS-COVERED GLACIERS; ENERGY BALANCE; GLACIER MODELLING; MORAINE FORMATION article 2015 ftumanchesterpub https://doi.org/10.3189/2015JoG14J235 2023-10-30T09:12:05Z In this paper we undertake a quantitative analysis of the dynamic process by which ice underneath a dry porous debris layer melts. We show that the incorporation of debris-layer airflow into a theoretical model of glacial melting can capture the empirically observed features of the so-called Østrem curve (a plot of the melt rate as a function of debris depth). Specifically, we show that the turning point in the Østrem curve can be caused by two distinct mechanisms: the increase in the proportion of ice that is debris-covered and/or a reduction in the evaporative heat flux as the debris layer thickens. This second effect causes an increased melt rate because the reduction in (latent) energy used for evaporation increases the amount of energy available for melting. Our model provides an explicit prediction for the melt rate and the temperature distribution within the debris layer, and provides insight into the relative importance of the two effects responsible for the maximum in the Østrem curve. We use the data of Nicholson and Benn (2006) to show that our model is consistent with existing empirical measurements. Article in Journal/Newspaper Journal of Glaciology The University of Manchester: Research Explorer Nicholson ENVELOPE(78.236,78.236,-68.612,-68.612) Østrem ENVELOPE(8.681,8.681,63.387,63.387) Journal of Glaciology 61 229 825 836 |
institution |
Open Polar |
collection |
The University of Manchester: Research Explorer |
op_collection_id |
ftumanchesterpub |
language |
English |
topic |
DEBRIS-COVERED GLACIERS; ENERGY BALANCE; GLACIER MODELLING; MORAINE FORMATION |
spellingShingle |
DEBRIS-COVERED GLACIERS; ENERGY BALANCE; GLACIER MODELLING; MORAINE FORMATION Evatt, Geoffrey Abrahams, I David Heil, Matthias Mayer, Christoph Kingslake, Jonathan Mitchell, Sarah L. Fowler, Andrew C. Clark, Christopher D. Glacial melt under a porous debris layer |
topic_facet |
DEBRIS-COVERED GLACIERS; ENERGY BALANCE; GLACIER MODELLING; MORAINE FORMATION |
description |
In this paper we undertake a quantitative analysis of the dynamic process by which ice underneath a dry porous debris layer melts. We show that the incorporation of debris-layer airflow into a theoretical model of glacial melting can capture the empirically observed features of the so-called Østrem curve (a plot of the melt rate as a function of debris depth). Specifically, we show that the turning point in the Østrem curve can be caused by two distinct mechanisms: the increase in the proportion of ice that is debris-covered and/or a reduction in the evaporative heat flux as the debris layer thickens. This second effect causes an increased melt rate because the reduction in (latent) energy used for evaporation increases the amount of energy available for melting. Our model provides an explicit prediction for the melt rate and the temperature distribution within the debris layer, and provides insight into the relative importance of the two effects responsible for the maximum in the Østrem curve. We use the data of Nicholson and Benn (2006) to show that our model is consistent with existing empirical measurements. |
format |
Article in Journal/Newspaper |
author |
Evatt, Geoffrey Abrahams, I David Heil, Matthias Mayer, Christoph Kingslake, Jonathan Mitchell, Sarah L. Fowler, Andrew C. Clark, Christopher D. |
author_facet |
Evatt, Geoffrey Abrahams, I David Heil, Matthias Mayer, Christoph Kingslake, Jonathan Mitchell, Sarah L. Fowler, Andrew C. Clark, Christopher D. |
author_sort |
Evatt, Geoffrey |
title |
Glacial melt under a porous debris layer |
title_short |
Glacial melt under a porous debris layer |
title_full |
Glacial melt under a porous debris layer |
title_fullStr |
Glacial melt under a porous debris layer |
title_full_unstemmed |
Glacial melt under a porous debris layer |
title_sort |
glacial melt under a porous debris layer |
publishDate |
2015 |
url |
https://research.manchester.ac.uk/en/publications/f0187075-9c62-4c10-8b3f-0ed497cb3cd5 https://doi.org/10.3189/2015JoG14J235 |
long_lat |
ENVELOPE(78.236,78.236,-68.612,-68.612) ENVELOPE(8.681,8.681,63.387,63.387) |
geographic |
Nicholson Østrem |
geographic_facet |
Nicholson Østrem |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Evatt , G , Abrahams , I D , Heil , M , Mayer , C , Kingslake , J , Mitchell , S L , Fowler , A C & Clark , C D 2015 , ' Glacial melt under a porous debris layer ' , Journal of Glaciology , vol. 61 , no. 229 , pp. 825-836 . https://doi.org/10.3189/2015JoG14J235 |
op_rights |
info:eu-repo/semantics/closedAccess |
op_doi |
https://doi.org/10.3189/2015JoG14J235 |
container_title |
Journal of Glaciology |
container_volume |
61 |
container_issue |
229 |
container_start_page |
825 |
op_container_end_page |
836 |
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1782336148834615296 |