This paper compares the performance of a conceptual modelling system and several physically-based models for predicting runo in a large hydrological basin, Tasersuaq, in west Greenland. This basin, which is typical of many Greenland basins, is interesting because of the fast hydrological response to
Snowmelt runoff modelling in an arid mountain watershed, Tarim Basin, China
โ Scribed by Xingong Li; Mark W. Williams
- Book ID
- 102266083
- Publisher
- John Wiley and Sons
- Year
- 2008
- Tongue
- English
- Weight
- 214 KB
- Volume
- 22
- Category
- Article
- ISSN
- 0885-6087
- DOI
- 10.1002/hyp.7098
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โฆ Synopsis
Abstract
The feasibility of simulating daily snowmelt runoff in an arid mountain watershed with limited hydroโmeteorological measurements was explored with an enhanced temperatureโindex snowmelt runoff model (SRM) in which the degreeโday factor (DDF) is varied on the basis of shortwave solar radiation and snow albedo. The model satisfactorily simulated snowmelt runoff with a model efficiency of 0ยท64 for the calibration year and efficiency values of 0ยท78 and 0ยท51 for two validation years. Analysis indicated that the model was sensitive to lapse rate and snow albedo parameterization. The distinct seasonal variation of lapse rate played a key role for successful simulation. Snow albedo parameterization, which directly scaled snow cover percentage into snow albedo, worked quite well for the watershed although further validation is needed. Eightโday snow cover data from the Moderate Resolution Imaging Spectroradiometer (MODIS) were used to feed the model. A frequency filter, which filtered out the clouds and large fluctuation of snow cover from the MODIS snow cover data, also improved model performance. The model, however, did not simulate peak stream flows well as most of the model runs underestimated them. Copyright ยฉ 2008 John Wiley & Sons, Ltd.
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