Property:Describe available test data
From CSDMS
This is a property of type Text.
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Db_dem.zip +
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Example outputs and associated wrapper scripts are available through the University of Virginia Dataverse at https://dx.doi.org/10.18130/V3/E0EGOC +
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Extensive input dataset is available on the CSDMS HPCC (beach) at '/scratch/ccny/RGISarchive' and '/scratch/saco2635/RGISarchiveCSDMS'. +
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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. +
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Global (GEMS-GLORI), regional, national and literature compilations. A subset used for validation. +
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Hillslope morphology data from the Dragon's Back Pressure Ridge is included in packaged code. +
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I have numerous data sets produced by an 8 processor Mac and a local unix cluster to confirm the model is initialized correctly. +
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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. +
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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. +
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MS thesis +
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Model test data are available through https://github.com/ajwdewit/pcse and described in https://doi.org/10.1016/j.agwat.2019.105746 +
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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. +
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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 +
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