Property:Describe time scale and resolution

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U
UMCESroms +
Hours, days, seasons. It also can be used for climate research (decades).  +
C
CBOFS2 +
Hours, days, seasons. It also can be used for climate research (decades).  +
CAM-CARMA +
I am running the model with dynamical time steps of 1800 seconds, but it only computes the radiative transfer every 200 timesteps.  +
Cyclopath +
Internal time step years to decades Model chron resolution 1000 years Total run time 1-10 My  +
A
AnugaSed +
Internal timestep is determined by ANUGA for numerical stability (in seconds). Output timestep is set by the user. Simulations are realistically limited to a few model hours.  +
M
Morphodynamic gravel bed +
It is applied for 90 years. The time step is ~0.7 days.  +
G
GullyErosionProfiler1D +
It is typically run for times no less than 25 years and no greater than 700 years.  +
W
WBMsed +
It simulate at daily time-steps. Maximum available datasets time-span is between 1901-present.  +
R
River Network Bed-Material Sediment +
Limited by computational resources.  +
N
Nitrate Network Model +
Limited by computational resources.  +
L
LISFLOOD +
Long-term water balance can be simulated (using a daily time step), as can individual flood events (using hourly time intervals, or even smaller). The output of a “water balance run” can be used to provide the initial conditions of a “flood run”.  +
G
GRLP +
Longer than the intermittency between channel-forming events  +
D
DeltaClassification +
Mapview at a given time  +
B
BITM +
Millennial scale  +
H
HydroTrend +
Minimal runtime: 1yr; up to > 10kyrs Daily discharge is the smallest output timestep  +
R
RiverMUSE +
Model constructed for daily time steps, but can be altered with little effort.  +
L
Lake-Permafrost with Subsidence +
Model needs daily (or smaller) timesteps.  +
C
CoastMorpho2D +
Morphological time steps can be on the order of years Time steps shorter than one tidal period are not realistic  +
G
GEOtop +
Most forcings are required at hourly scale. Integration time step is what required by numerical algorithms to converge (depends actually on processes)  +
D
DeltaSIM +
Mostly tested for Holocene applications (>10,000yrs), potentially longer time scales.  +
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