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Snowmelt runoff decreases.
In August, snowmelt runoff from non-glacierized regions of the catchment is small, while bare ice melt is most important.
The depressions stored most of the snowmelt runoff generated within their respective watersheds.
Snowmelt runoff from each watershed was measured with two flumes with overlapping ranges arranged in series.
Streamflow trends were detected by Mann-Kendall tests and changes in snowmelt runoff timing were analyzed based on the winter/spring snowmelt runoff center time (WSCT).
Streamflow and snowmelt runoff timing of mountain rivers are susceptible to climate change.
Nonetheless, snowmelt runoff and Rs played more substantial roles than precipitation in the snowmelt period.
Methods for estimating the hydrometeorlogical fluxes, evapotranspiration and snowmelt runoff, using these state variables are also described.
A temperature index based snowmelt runoff model is used to simulate basin runoff from the year 2000 to 2059.
Accounting for the actual signature of snowmelt runoff has strong effects on its perceived role in recharging groundwater.
Moreover, the results are compared with that of a conceptual model, Snowmelt Runoff Model (SRM), application using SCA as an input.
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