Property:Describe numerical limitations

From CSDMS

This is a property of type Text.

Showing 20 pages using this property.
H
As the size of the DEM increases, processing time will increase. An 8000*8000 DEM will take several days to process. Documentation is available to help users select appropriate input parameters.  +
B
Assumes Bingham rheology  +
S
Assumes constant flexural rigidity  +
C
Assumes mixed-grain sediment compacts linearly  +
F
At the present I am trying to improve the wetting and drying algorithm, unphysical large velocities are sometime produced at the wet/dry front.  +
B
Becomes unstable at timesteps much greater than 10 years.  +
S
Becomes very slow if run on domains with pits. Options include filling pits before running the model, or using the Landlab DepressionFinderAndRouter.  +
G
Can be very slow in complex systems.  +
Catchment must be small enough that it can be approximated as being flat.  +
A
Code is research grade  +
P
Code is research grade  +
G
Concerns about extrapolations beyond range of data used for model calibration and parameterization.  +
W
Covergency and instabiliy may occur depending the stiffness of the problems.  +
Q
Currently it is not possible to model transgression followed by regression.  +
G
Currently only shallow water equations are solved, using explicit finite volume methods. High order Boussinesq equations to better model dispersive waves (e.g. for short wavelength submarine landslide generated tsunamis) would require implicit time stepping and is still in the experimental phase.  +
E
D8 flow codes are used to compute contributing areas. Would be better to use D-Infinity or the Mass-Flux method.  +
L
Depends on application/process  +
P
Depends only on computer resources.  +
C
Diffusion and other sediment transport routines require short time steps  +
G
Documentation provides a description of the available processes and associated limitations: https://gospl.readthedocs.io/en/latest/tech_guide/index.html  +