The Radiation Budget of a Subarctic Woodland Canopy

Open woodland is a major sub-type of the circum global boreal forest zone. In Canada it dominates the basins of a number of large hydroelectric schemes in which snowmelt is a critical phase of the hydrologic cycle. The forest vegetation strongly influences the radiant energy flux to the snow and is...

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Published in:ARCTIC
Main Authors: Lafleur, Peter, Adams, Peter
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1986
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65118
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/65118 2023-05-15T14:19:14+02:00 The Radiation Budget of a Subarctic Woodland Canopy Lafleur, Peter Adams, Peter 1986-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65118 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65118/49032 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65118 ARCTIC; Vol. 39 No. 2 (1986): June: 109–194; 172-176 1923-1245 0004-0843 Forest ecology Forests Radiation budgets Runoff Snowmelt Middle North info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1986 ftunivcalgaryojs 2022-03-22T21:22:12Z Open woodland is a major sub-type of the circum global boreal forest zone. In Canada it dominates the basins of a number of large hydroelectric schemes in which snowmelt is a critical phase of the hydrologic cycle. The forest vegetation strongly influences the radiant energy flux to the snow and is therefore important in the production of snowmelt runoff and its prediction. The radiation budget of a subarctic open woodland canopy in northern Quebec is computed from measurements of net allwave, solar and longwave radiation components over the snowpack at treeless and woodland sites. The canopy gains solar radiation both directly and from solar radiation reflected off the snowpack, the latter enhanced by the larger spacing between tree crowns. Canopy heating from absorbed solar radiation leads to a considerable longwave flux being emitted by the tree crowns. Overall, the radiant energy exchange in the open woodland behaves differently than for a closed crown forest. This is believed to be a function of a variety of canopy characteristics, not solely of tree crown density.Key Words: snowmelt, open woodland, radiation budget, northern Quebec Mots clés: fonte des neiges, forêt claire, taux de rayonnement, nord du Québec Article in Journal/Newspaper Arctic Subarctic University of Calgary Journal Hosting Canada ARCTIC 39 2
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic Forest ecology
Forests
Radiation budgets
Runoff
Snowmelt
Middle North
spellingShingle Forest ecology
Forests
Radiation budgets
Runoff
Snowmelt
Middle North
Lafleur, Peter
Adams, Peter
The Radiation Budget of a Subarctic Woodland Canopy
topic_facet Forest ecology
Forests
Radiation budgets
Runoff
Snowmelt
Middle North
description Open woodland is a major sub-type of the circum global boreal forest zone. In Canada it dominates the basins of a number of large hydroelectric schemes in which snowmelt is a critical phase of the hydrologic cycle. The forest vegetation strongly influences the radiant energy flux to the snow and is therefore important in the production of snowmelt runoff and its prediction. The radiation budget of a subarctic open woodland canopy in northern Quebec is computed from measurements of net allwave, solar and longwave radiation components over the snowpack at treeless and woodland sites. The canopy gains solar radiation both directly and from solar radiation reflected off the snowpack, the latter enhanced by the larger spacing between tree crowns. Canopy heating from absorbed solar radiation leads to a considerable longwave flux being emitted by the tree crowns. Overall, the radiant energy exchange in the open woodland behaves differently than for a closed crown forest. This is believed to be a function of a variety of canopy characteristics, not solely of tree crown density.Key Words: snowmelt, open woodland, radiation budget, northern Quebec Mots clés: fonte des neiges, forêt claire, taux de rayonnement, nord du Québec
format Article in Journal/Newspaper
author Lafleur, Peter
Adams, Peter
author_facet Lafleur, Peter
Adams, Peter
author_sort Lafleur, Peter
title The Radiation Budget of a Subarctic Woodland Canopy
title_short The Radiation Budget of a Subarctic Woodland Canopy
title_full The Radiation Budget of a Subarctic Woodland Canopy
title_fullStr The Radiation Budget of a Subarctic Woodland Canopy
title_full_unstemmed The Radiation Budget of a Subarctic Woodland Canopy
title_sort radiation budget of a subarctic woodland canopy
publisher The Arctic Institute of North America
publishDate 1986
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65118
geographic Canada
geographic_facet Canada
genre Arctic
Subarctic
genre_facet Arctic
Subarctic
op_source ARCTIC; Vol. 39 No. 2 (1986): June: 109–194; 172-176
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65118/49032
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65118
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