On glacier energy balance, ablation, and air temperature.
Tries to reconcile the facts that there are often useful correlations between ablation or run-off and air temperature while net radiation is usually the major source of ablation energy. As examples, statistics are evaluated for four published series from Arctic Canada. Although the net radiation is...
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ftumanchesterpub:oai:pure.atira.dk:publications/e12a734b-4d05-4944-83de-4099762f86c7 2023-11-12T04:13:04+01:00 On glacier energy balance, ablation, and air temperature. Braithwaite, R. J. 1981 https://research.manchester.ac.uk/en/publications/e12a734b-4d05-4944-83de-4099762f86c7 eng eng info:eu-repo/semantics/restrictedAccess Braithwaite , R J 1981 , ' On glacier energy balance, ablation, and air temperature. ' , Journal of Glaciology , vol. 27 , no. 97 , pp. 381-391 . article 1981 ftumanchesterpub 2023-10-30T09:17:45Z Tries to reconcile the facts that there are often useful correlations between ablation or run-off and air temperature while net radiation is usually the major source of ablation energy. As examples, statistics are evaluated for four published series from Arctic Canada. Although the net radiation is the largest energy source in all four cases, the ablation rate is moderately well correlated with temperature and poorly correlated with net radiation. This is because the sensible heat flux is more variable than the radiation in three cases and is itself better correlated with temperature in all four cases. The major contributions to the increase of ablation rate with temperature (on average 6.3kg m-2 d-1 deg-1) are due to sensible heat, followed by latent heat with a small contribution from net radiation. The resulting ablation-temperature model explains about half the variance of ablation rate. The main application of such a simple model is for the estimation of ablation totals in areas where glaciological and hydrological data are sparse. -Author Article in Journal/Newspaper Arctic glacier* Journal of Glaciology The University of Manchester: Research Explorer Arctic Canada |
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Open Polar |
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The University of Manchester: Research Explorer |
op_collection_id |
ftumanchesterpub |
language |
English |
description |
Tries to reconcile the facts that there are often useful correlations between ablation or run-off and air temperature while net radiation is usually the major source of ablation energy. As examples, statistics are evaluated for four published series from Arctic Canada. Although the net radiation is the largest energy source in all four cases, the ablation rate is moderately well correlated with temperature and poorly correlated with net radiation. This is because the sensible heat flux is more variable than the radiation in three cases and is itself better correlated with temperature in all four cases. The major contributions to the increase of ablation rate with temperature (on average 6.3kg m-2 d-1 deg-1) are due to sensible heat, followed by latent heat with a small contribution from net radiation. The resulting ablation-temperature model explains about half the variance of ablation rate. The main application of such a simple model is for the estimation of ablation totals in areas where glaciological and hydrological data are sparse. -Author |
format |
Article in Journal/Newspaper |
author |
Braithwaite, R. J. |
spellingShingle |
Braithwaite, R. J. On glacier energy balance, ablation, and air temperature. |
author_facet |
Braithwaite, R. J. |
author_sort |
Braithwaite, R. J. |
title |
On glacier energy balance, ablation, and air temperature. |
title_short |
On glacier energy balance, ablation, and air temperature. |
title_full |
On glacier energy balance, ablation, and air temperature. |
title_fullStr |
On glacier energy balance, ablation, and air temperature. |
title_full_unstemmed |
On glacier energy balance, ablation, and air temperature. |
title_sort |
on glacier energy balance, ablation, and air temperature. |
publishDate |
1981 |
url |
https://research.manchester.ac.uk/en/publications/e12a734b-4d05-4944-83de-4099762f86c7 |
geographic |
Arctic Canada |
geographic_facet |
Arctic Canada |
genre |
Arctic glacier* Journal of Glaciology |
genre_facet |
Arctic glacier* Journal of Glaciology |
op_source |
Braithwaite , R J 1981 , ' On glacier energy balance, ablation, and air temperature. ' , Journal of Glaciology , vol. 27 , no. 97 , pp. 381-391 . |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1782331243746033664 |