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Assimilation of snow cover and snow depth into a snow model to estimate snow water equivalent and snowmelt runoff in a Himalayan catchment

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Figure

Figure 1. Study area with the locations of the in situ observations.Langtang and Langshisha refer to the two main glaciers in the upperLangtang valley.
Table 1. Overview of the in situ observations and their specifications. Locations are shown in Fig
Table 2. Parameters in the snow model. Initial value indicates the uncalibrated parameter value and the value range indicates the range whichis used for the sensitivity analysis
Figure 3. Observed surface temperature with 10 min interval at twolocations (Table 1)
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