A comparison study of two snow models using data from different Alpine sites

Finally, we compared the results of ARPS simulations with results from the terrain-based parameter and assess its ability to reproduce spatial patterns of snow distribution. Figure

Bi- ases may be due to uncertainty of the boundary conditions from the ERA-Interim reanalysis (Chaudhuri et al., 2013) since errors from the WRF downscaling model are difficult

The aim of the study was to investigate the relative performance of the Snowmelt Runoff Model (SRM) to simulate streamflow in five sub-catchments of the High Atlas Mountain

Here we calibrate and evaluate a simple empirical function to estimate the fractional snow cover (FSC) in open terrains using the normalized difference snow index (NDSI) from 20

We used both in situ and remote sensing data to assess both Aqua and Terra MODIS daily snow cover binary products (snow/no snow) in the Pyrenees.. For the first time, we as- sembled

The results will be discussed in terms of: (a) availability and potential of MODIS snow cover data for identifying RSLE changes during snowmelt runoff events, (b) spatial and

Now that a relation between the threshold friction velocity and the diameter of the po- tentially mobilized particles is available, the friction velocity in a powder snow avalanche

Considering Sherbrooke-A snow depth data to be representative, it becomes obvious that using SIRENE data did not provide accurate thickness simulations Table 4; however, results