Transportation, sublimation and accumulation of snow dominate snow cover development in the Arctic and produce episodic high evaporative ยฏuxes. Unfortunately, blowing snow processes are not presently incorporated in any hydrological or meteorological models. To demonstrate the application of simple
A distributed model of blowing snow over complex terrain
โ Scribed by Richard Essery; Long Li; John Pomeroy
- Book ID
- 102658969
- Publisher
- John Wiley and Sons
- Year
- 1999
- Tongue
- English
- Weight
- 901 KB
- Volume
- 13
- Category
- Article
- ISSN
- 0885-6087
No coin nor oath required. For personal study only.
โฆ Synopsis
Physically-based models of blowing snow and windยฏow are used to develop a distributed model of blowing snow transport and sublimation over complex terrain. The model is applied to an arctic tundra basin. A reasonable agreement with results from snow surveys is obtained, provided sublimation processes are included; a simulation without sublimation produces much greater snow accumulations than were measured. The model is able to reproduce some observed features of redistributed snowcovers: distributions of snow mass, classiยฎed by vegetation type and landform, can be approximated by lognormal distributions, and standard deviations of snow mass along transects follow a power law with transect length up to a cut-o. The representation used for the downwind development of blowing snow with changes in windspeed and surface characteristics is found to have a large moderating inยฏuence on snow redistribution.
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