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|Storage:||The size of this resource is 4.7 MB|
|Created:||Apr 12, 2018 at 6:09 p.m.|
|Last updated:|| Jun 08, 2018 at 3:58 a.m.
|Citation:||See how to cite this resource|
|Content types:||Model Instance Content|
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Six headwater catchments of the Gwynns Falls watershed, located in Baltimore County, Maryland, USA, were simulated using ParFlow.CLM. We utilized a 10-m horizontal gridding, with catchment areas ranging on the order of 0.2 to 2 sq. km. Vertical discretization was variable ranging from 0.1 to 8m with the terrain-following grid feature of ParFlow.CLM activated. Model domains contained 69,120 to 505,440 finite difference cells. The simulation period was 1 January 2012 to 31 December 2015.
Each compressed tar archive (.tar.gz) contains the inputs required to execute the model run. These include: ParFlow binary files (.pfb) for permeability, slope and geologic unit indicator field, CLM text files (.dat and .txt) for input paramaters, 1-D NLDAS2 forcing, vegetation matrix and vegetation parameters, and a ParFlow input tcl file to generate model input database (.tcl). A Bash shell script (.sh) containing model dimensions is also included.
|MIGRATED_FROM||Model Instance Resource|
|Title||Owners||Sharing Status||My Permission|
|ParFlow.CLM model input files of six headwater catchments of the Gwynns Falls watershed, Baltimore County, Maryland, USA||Michael Barnes||Published||Open Access|
This resource was created using funding from the following sources:
|Agency Name||Award Title||Award Number|
|National Science Foundation||Collaborative Research, WSC-Category 2: Regional Climate Variability and Patterns of Urban Development - Impacts on the Urban Water Cycle and Nutrient Export||CBET-1058038|
People or Organizations that contributed technically, materially, financially, or provided general support for the creation of the resource's content but are not considered authors.
|Claire Welty||University of Maryland; Baltimore County||US|
|Andrew J Miller||University of Maryland; Baltimore County||US|
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.http://creativecommons.org/licenses/by/4.0/
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