Multiscale modelling of snow depth over an agricultural field in a small catchement in southern ontario, canada.
Snow is a common overlying surface during winter-time and the redistribution of snow by wind is a very important concept for any hydrological research project located within the cryosphere. Wind redistributes snow by eroding it from areas of high wind speed, such as ridge tops and windward slopes, a...
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| Language: | en |
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2011
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| Online Access: | http://hdl.handle.net/10012/5970 |