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Evaluation and bias correction of SNODAS snow water equivalent (SWE) for streamflow simulation in eastern Canadian basins
Authors:Zahra Zahmatkesh  Dominique Tapsoba  James Leach  Paulin Coulibaly
Institution:1. Department of Civil Engineering, McMaster University, Hamilton, Ontario, Canadazhr_zahmatkesh@yahoo.com;3. Géostatistique, Institut de recherche d’Hydro-Québec, Varennes, Quebec, Canada;4. Department of Civil Engineering, McMaster University, Hamilton, Ontario, Canada;5. Department of Civil Engineering/School of Geography and Earth Sciences, McMaster University, Hamilton, Ontario, Canada
Abstract:ABSTRACT

In snow-dominated basins, collection of snow data while capturing its spatio-temporal variability is difficult; therefore, integrating assimilation products could be a viable alternative for improving streamflow simulation. This study evaluates the accuracy of daily snow water equivalent (SWE) provided by the SNOw Data Assimilation System (SNODAS) of the National Weather Service at a 1-km2 resolution for two basins in eastern Canada, where SWE is a critical variable intensifying spring runoff. A geostatistical interpolation method was used to distribute snow observations. SNODAS SWE products were bias-corrected by matching their cumulative distribution function to that of the interpolated snow. The corrected SWE was then used in hydrological modelling for streamflow simulation. The results indicate that the bias-correction method significantly improved the accuracy of the SNODAS products. Moreover, the corrected SWE improved the simulation performance of the peak values. Although the uncertainty of SNODAS estimates is high for eastern Canadian basins, they are still of great value for regions with few snow stations.
Keywords:SNODAS  SWE  eastern Canadian basins  spatial interpolation  bias correction  streamflow simulation
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