Tags: openstreams/wflow
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2019.1 - Wflow\_sbm, redesign of lateral subsurface flow because of a bug that resulted in an overestimation of lateral subsurface flux: - The kinematic wave approach is used to route subsurface flow laterally. - Kinematic wave solution for surface (overland and river) and subsurface flow added to wflow\_funcs, and used by wflow\_sbm. Numba (open-source JIT compiler) is used to accelerate these functions. This replaces the PCRaster kinematic wave solution. - A seperate kinematic wave reservoir for river (self.RiverRunoff) and overland flow (self.LandRunoff) - Lateral subsurface flow and overland flow feed into drainage network (channel) based on ratio slopes (slope upstream cell / (slope upstream cell + slope cell)) - Option to provide land slope and river slope (staticmaps) - Removed sub-grid runoff generation - Removed re-infiltration of surface water - Wflow\_hbv uses kinematic wave solution for surface flow available in wflow\_funcs (replacement of PCRaster kinematic wave solution) - Option to enable iteration (smaller time steps) for kinematic wave solution for surface runoff (wflow\_hbv and wflow\_sbm) - Added hydrological model wflow\_w3 to wflow framework, based on Australian Water Resources Assessment Landscape model (AWRA-L), an improved version compared to wflow\_W3RA. - Added hydrological model wflow\_stream to wflow framework (STREAM (Spatial Tools for River Basins and Environment and Analysis of Management Options)). - Added experimental version of wflow\_sediment to simulate soil erosion and delivery to the river system. - Added the wflow\_emwaq module: provides a set of functions to create and link a Delft3D-WAQ or D-Emission model to a wflow model. - Update of lake modelling for wflow\_hbv and wflow\_sbm (including also Modified Puls Approach) in wflow\_funcs - Update of glacier model (used by wflow\_hbv and wflow\_sbm) - Parameter Manning N of river can be linked to streamorder for wflow\_hbv - setuptools_scm used for version wflow package
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