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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