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Type: | Resource | |
Storage: | The size of this resource is 6.4 MB | |
Created: | Apr 18, 2023 at 2:23 p.m. | |
Last updated: | May 12, 2023 at 2:25 p.m. | |
Citation: | See how to cite this resource |
Sharing Status: | Public |
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Views: | 398 |
Downloads: | 10 |
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Abstract
These are the datasets used in the paper by Kirker, A N, and L Toran. 2023. We used the distributed hydrologic model GSSHA to simulate overland runoff from impervious and semi-pervious (low vegetation) land covers in a 0.3 km2 urban catchment. To track the arrival of water to a stormwater basin inlet from distinct parts of the catchment, we applied a conservative solute tracer to portions of the gridded model area. These data show the variability in discharge amount and solute arrival for modeled scenarios with different slopes, land uses, and precipitation amounts. A full model run has also been included in the .zip file so that users of Aquavevo's WMS may replicate these results.
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Credits
Funding Agencies
This resource was created using funding from the following sources:
Agency Name | Award Title | Award Number |
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William Penn Foundation | 39–18 |
Contributors
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.
Name | Organization | Address | Phone | Author Identifiers |
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Robert Ryan | Temple University |
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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