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StreamFlow 1.0: an extension to the spatially distributed snow model Alpine3D for hydrological modelling and deterministic stream temperature prediction

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Figure

Table 1. List of semi-distributed hydrological models which simulate both stream discharge and stream temperature and have been reviewedin the context of the present study.
Figure 1. Schematic representation of the work flow in StreamFlow. Note that the first two steps are not performed in StreamFlow itself butin Alpine3D and with the help of TauDEM, respectively.
Figure 2. Available methods for spatially discretizing the streamreaches in StreamFlow: (a) the lumped approach, treating eachstream reach as a lumped entity, and (b) the discretized approach,subdividing each reach into smaller entities called cells
Fig. 3b. Class Implementation defines the interface to be im-plemented by all the subclasses computing discharge, whileclass Decorator corresponds to the parent of all classes fo-
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