Snowmelt energy balance in a burned forest plot, Crowsnest Pass, Alberta, Canada
Forested headwater basins in western North America are subject to major change from natural and anthropogenic disturbance, including wildfire, insect infestation, disease, and forest harvesting. These changes have subsequent impacts on sub‐canopy snow processes, particularly snow accumulation and me...
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| Published in | Hydrological processes Vol. 25; no. 19; pp. 3012 - 3029 |
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| Main Authors | , |
| Format | Journal Article |
| Language | English |
| Published |
Chichester, UK
John Wiley & Sons, Ltd
15.09.2011
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| Subjects | |
| Online Access | Get full text |
| ISSN | 0885-6087 1099-1085 1099-1085 |
| DOI | 10.1002/hyp.8067 |
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| Summary: | Forested headwater basins in western North America are subject to major change from natural and anthropogenic disturbance, including wildfire, insect infestation, disease, and forest harvesting. These changes have subsequent impacts on sub‐canopy snow processes, particularly snow accumulation and melt, with cascading effects on downstream systems. We apply a simple, process‐based point energy balance model to quantify differences in energy balance characteristics between a burned and a control plot. In the burned plot, more snow accumulated on the ground surface, there was more energy available for snowmelt, the snow melted more rapidly, and complete snowpack removal occurred sooner than in the control plot. Although results are comparable to cleared forest stands, standing dead trees in burned forest stands attenuate incoming short‐wave radiation, wind speed, temperature, and snow accumulation on the surface to a greater degree than is observed in cleared stands. |
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| Bibliography: | http://dx.doi.org/10.1002/hyp.8067 istex:3FC0FB34EA4546AB46B3CA60E81AC4222538C818 ark:/67375/WNG-G42BLKK3-M ArticleID:HYP8067 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
| ISSN: | 0885-6087 1099-1085 1099-1085 |
| DOI: | 10.1002/hyp.8067 |