Property:Describe available test data

From CSDMS

This is a property of type Text.

Showing 50 pages using this property.
F
AMASSED; STRATAFORM; EUROSTRATAFORM  +
A
AquaTellUs was originally developed for simulation of the fluvial-dominated Volga delta. The 2D experiments are still available and can be used as a test data set.  +
I
As an example of running IDA, and a test to ensure that it is running correctly, a small project is provided. Unpack it using tar -xjf example.tar.bz2 Files: dir.bin: flow directions for a 1000 x 1000 cell landscape true.bin: the correct answer, for comparison run.sh: a Bash script to run the example. The script must be modified to specify the path to the IDA executable. Running: Make the Bash script executable with the command chmod +x run.sh Run the Bash script with ./run.sh It will run IDA several times with different options, and may take some time Depending on your configuration of PETSc, some of the runs may fail  +
T
Available test data sets: * Treynor watershed, in the Nishnabotna River basin, Iowa, USA. * (Two large rainfall events.) * Small basin in Kentucky. * Inclined plane for testing. * Arctic watershed data from Larry Hinzman (UAF). * See /data/progs/topoflow/3.0/data on CSDMS cluster.  +
Available test data sets: * Treynor watershed, in the Nishnabotna River basin, Iowa, USA. * (Two large rainfall events.) * Small basin in Kentucky. * Inclined plane for testing. * Arctic watershed data from Larry Hinzman (UAF). * See /data/progs/topoflow/3.0/data on CSDMS cluster.  +
Available test data sets: * Treynor watershed, in the Nishnabotna River basin, Iowa, USA. * (Two large rainfall events.) * Small basin in Kentucky. * Inclined plane for testing. * Arctic watershed data from Larry Hinzman (UAF). * See /data/progs/topoflow/3.0/data on CSDMS cluster.  +
Available test data sets: *Treynor watershed, in the Nishnabotna River basin, Iowa, USA. * (Two large rainfall events.) *Small basin in Kentucky. *Inclined plane for testing. *Arctic watershed data from Larry Hinzman (UAF). *See /data/progs/topoflow/3.0/data on CSDMS cluster.  +
Available test data sets: *Treynor watershed, in the Nishnabotna River basin, Iowa, USA. * (Two large rainfall events.) *Small basin in Kentucky. *Inclined plane for testing. *Arctic watershed data from Larry Hinzman (UAF). *See /data/progs/topoflow/3.0/data on CSDMS cluster.  +
Available test data sets: *Treynor watershed, in the Nishnabotna River basin, Iowa, USA. * (Two large rainfall events.) *Small basin in Kentucky. *Inclined plane for testing. *Arctic watershed data from Larry Hinzman (UAF). *See /data/progs/topoflow/3.0/data on CSDMS cluster.  +
Available test data sets: *Treynor watershed, in the Nishnabotna River basin, Iowa, USA. * (Two large rainfall events.) *Small basin in Kentucky. *Inclined plane for testing. *Arctic watershed data from Larry Hinzman (UAF). *See /data/progs/topoflow/3.0/data on CSDMS cluster.  +
Available test data sets: *Treynor watershed, in the Nishnabotna River basin, Iowa, USA. * (Two large rainfall events.) *Small basin in Kentucky. *Inclined plane for testing. *Arctic watershed data from Larry Hinzman (UAF). *See /data/progs/topoflow/3.0/data on CSDMS cluster.  +
Available test data sets: *Treynor watershed, in the Nishnabotna River basin, Iowa, USA. * (Two large rainfall events.) *Small basin in Kentucky. *Inclined plane for testing. *Arctic watershed data from Larry Hinzman (UAF). *See /data/progs/topoflow/3.0/data on CSDMS cluster.  +
Available test data sets: *Treynor watershed, in the Nishnabotna River basin, Iowa, USA. * (Two large rainfall events.) *Small basin in Kentucky. *Inclined plane for testing. *Arctic watershed data from Larry Hinzman (UAF). *See /data/progs/topoflow/3.0/data on CSDMS cluster.  +
Available test data sets: *Treynor watershed, in the Nishnabotna River basin, Iowa, USA. * (Two large rainfall events.) *Small basin in Kentucky. *Inclined plane for testing. *Arctic watershed data from Larry Hinzman (UAF). *See /data/progs/topoflow/3.0/data on CSDMS cluster.  +
Available test data sets: *Treynor watershed, in the Nishnabotna River basin, Iowa, USA. * (Two large rainfall events.) *Small basin in Kentucky. *Inclined plane for testing. *Arctic watershed data from Larry Hinzman (UAF). *See /data/progs/topoflow/3.0/data on CSDMS cluster.  +
Available test data sets: *Treynor watershed, in the Nishnabotna River basin, Iowa, USA. * (Two large rainfall events.) *Small basin in Kentucky. *Inclined plane for testing. *Arctic watershed data from Larry Hinzman (UAF). *See /data/progs/topoflow/3.0/data on CSDMS cluster.  +
Available test data sets: *Treynor watershed, in the Nishnabotna River basin, Iowa, USA. * (Two large rainfall events.) *Small basin in Kentucky. *Inclined plane for testing. *Arctic watershed data from Larry Hinzman (UAF). *See /data/progs/topoflow/3.0/data on CSDMS cluster.  +
Available test datat sets: *Treynor watershed, in the Nishnabotna River basin, Iowa, USA. (Two large rainfall events.) *Small basin in Kentucky. *Inclined plane for testing. *Arctic watershed data from Larry Hinzman (UAF). *See /data/progs/topoflow/3.0/data on CSDMS cluster.  +
C
Burgess (2008)  +
D
Caspian sea experiences extremely rapid sea level fluctuation, making it a great test data set for coastline shifts.  +
G
Cropland area for ...  +
H
T
Example of TOPMODEL simulation  +
S
Example outputs and associated wrapper scripts are available through the University of Virginia Dataverse at https://dx.doi.org/10.18130/V3/E0EGOC  +
M
Example runs for most types of simulation scenarios  +
W
Extensive input dataset is available on the CSDMS HPCC (beach) at '/scratch/ccny/RGISarchive' and '/scratch/saco2635/RGISarchiveCSDMS'.  +
R
Flow velocities measured under current conditions in the Everglades in ridge (high-flow-resistance) and slough (low-flow-resistance) vegetation communities. This is very limited validation, as it only tests simulated velocities at the low end of the range of velocities the model is capable of simulating. Results are shown in Larsen and Harvey, Geomorphology, 2010, Fig. 4.  +
S
For example : Test of the non-hydrostatic version with water tank experiments.  +
For now only a basic synthetic surface.  +
G
Global (GEMS-GLORI), regional, national and literature compilations. A subset used for validation.  +
1
Hillslope morphology data from the Dragon's Back Pressure Ridge is included in packaged code.  +
W
I have numerous data sets produced by an 8 processor Mac and a local unix cluster to confirm the model is initialized correctly.  +
B
In order to verify the millennial-scale evolution of a barrier island, it is necessary to know the sea level curve, the rate of lagoonal deposition, the rate of overwash and the initial shelf profile. The BIT Model has been applied to the shelf profile in front of Sand Key, Florida.  +
H
Input data used in the preparation of the associated manuscript is all available from www.opentopography.org along with all processing and visualization code at https://github.com/sgrieve/LH_Paper_Plotting so users can compare their results with those contained within the manuscript.  +
1
W
Model test data are available through https://github.com/ajwdewit/pcse and described in https://doi.org/10.1016/j.agwat.2019.105746  +
S
Model was only used for modeling coastline change in the vicinity of Barrow, Alaska. Hourly wind data from a met station at the Barrow Airport was used to drive the model. High-resolution coastline data digitized from aerial photos by Manley et al. (2006) was used for initial and final coastlines. The latter was used for validation purposes. High-resolution DEMs were also used.  +
R
Modeling testing performed on data from the lower Colorado River and North Fork Toutle River. Model input data available here: https://github.com/rodlammers/REM  +
H
N/A  +
F
N/A  +
I
Nightly runs are carried out on every SVN repository commit.  +
M
None at present - forthcoming  +
G
None available  +
W
ONR test bed and others.  +
P
ParFlow contains a directory of test cases that may be automated as a check of the code.  +
L
Permafrost model can be tested with ground temperature time series at several depths. Lake model can be tested with known ice depths (though snow, not accounted for in model, can affect depth by several 10s of cm).  +
G
Please look at the GEOtop website: http://www.slideshare.net/GEOFRAMEcafe/geotop-2008?type=powerpoint  +
C
Q(m^3/s): daily water discharge series, 365 by 1 matrix Qs(kg/s): daily sediment flux series, 365 by 1 matrix The trigger flood event is set at the 232th day  +
G
Sample input and output files are included with the code.  +
Sample input files used to create plots shown in manual.  +