Effect of glaciers on annual run-off, Johan Dahl Land, south Greenland
Run-off data for two basins one of which contains glaciers, are compared with precipitation at a nearby weather station and with ablation measured in the glacier basin. Seasonal variations of run-off for the two basins are broadly similar while run-off from the glacier basin has smaller year-to-year...
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ftumanchesterpub:oai:pure.atira.dk:publications/8d1d4ed5-175f-42a1-a9b7-04e507e2d9ba 2023-11-12T04:17:26+01:00 Effect of glaciers on annual run-off, Johan Dahl Land, south Greenland Braithwaite, R. J. Olesen, O. B. 1988 https://research.manchester.ac.uk/en/publications/8d1d4ed5-175f-42a1-a9b7-04e507e2d9ba eng eng info:eu-repo/semantics/restrictedAccess Braithwaite , R J & Olesen , O B 1988 , ' Effect of glaciers on annual run-off, Johan Dahl Land, south Greenland ' , Journal of Glaciology , vol. 34 , no. 117 , pp. 200-207 . article 1988 ftumanchesterpub 2023-10-30T09:12:17Z Run-off data for two basins one of which contains glaciers, are compared with precipitation at a nearby weather station and with ablation measured in the glacier basin. Seasonal variations of run-off for the two basins are broadly similar while run-off from the glacier basin has smaller year-to-year variations. A simple statistical model shows that this is the result of a negative correlation between ablation and precipitation, which has the effect of reducing run-off variations in basins with a moderate amount of glacier for highly glacierized basins. The model also predicts an increasing run-off with ablation correlation and a decreasing run-off with precipitation correlation as the amount of glacier cover increases. -from Authors Article in Journal/Newspaper glacier Greenland Journal of Glaciology The University of Manchester: Research Explorer Greenland |
institution |
Open Polar |
collection |
The University of Manchester: Research Explorer |
op_collection_id |
ftumanchesterpub |
language |
English |
description |
Run-off data for two basins one of which contains glaciers, are compared with precipitation at a nearby weather station and with ablation measured in the glacier basin. Seasonal variations of run-off for the two basins are broadly similar while run-off from the glacier basin has smaller year-to-year variations. A simple statistical model shows that this is the result of a negative correlation between ablation and precipitation, which has the effect of reducing run-off variations in basins with a moderate amount of glacier for highly glacierized basins. The model also predicts an increasing run-off with ablation correlation and a decreasing run-off with precipitation correlation as the amount of glacier cover increases. -from Authors |
format |
Article in Journal/Newspaper |
author |
Braithwaite, R. J. Olesen, O. B. |
spellingShingle |
Braithwaite, R. J. Olesen, O. B. Effect of glaciers on annual run-off, Johan Dahl Land, south Greenland |
author_facet |
Braithwaite, R. J. Olesen, O. B. |
author_sort |
Braithwaite, R. J. |
title |
Effect of glaciers on annual run-off, Johan Dahl Land, south Greenland |
title_short |
Effect of glaciers on annual run-off, Johan Dahl Land, south Greenland |
title_full |
Effect of glaciers on annual run-off, Johan Dahl Land, south Greenland |
title_fullStr |
Effect of glaciers on annual run-off, Johan Dahl Land, south Greenland |
title_full_unstemmed |
Effect of glaciers on annual run-off, Johan Dahl Land, south Greenland |
title_sort |
effect of glaciers on annual run-off, johan dahl land, south greenland |
publishDate |
1988 |
url |
https://research.manchester.ac.uk/en/publications/8d1d4ed5-175f-42a1-a9b7-04e507e2d9ba |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
glacier Greenland Journal of Glaciology |
genre_facet |
glacier Greenland Journal of Glaciology |
op_source |
Braithwaite , R J & Olesen , O B 1988 , ' Effect of glaciers on annual run-off, Johan Dahl Land, south Greenland ' , Journal of Glaciology , vol. 34 , no. 117 , pp. 200-207 . |
op_rights |
info:eu-repo/semantics/restrictedAccess |
_version_ |
1782334333789405184 |