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|Created:||Nov 12, 2020 at 3:10 a.m.|
|Last updated:|| Jan 29, 2021 at 9:42 p.m.
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Miscellaneous shapefiles associated with the development and analysis of the 2D HEC-RAS model from
Czuba, J.A., S.R. David, D.A. Edmonds, and A.S. Ward (2019), Dynamics of surface-water connectivity in a low-gradient meandering river floodplain, Water Resources Research, 55(3), 1849-1870, https://doi.org/10.1029/2018WR023527
AOI.shp -- Area of Interest, extent of inundation for the largest flow.
digi_banklines.shp -- hand-digitized top of bank along left and right banks in the AOI.
domainCL.shp -- river centerline through the entire model domain.
|This resource is referenced by||Czuba, J.A., S.R. David, D.A. Edmonds, and A.S. Ward (2019), Dynamics of surface-water connectivity in a low-gradient meandering river floodplain, Water Resources Research, 55(3), 1849-1870, https://doi.org/10.1029/2018WR023527|
|This resource is referenced by||David, S.R., J.A. Czuba, D.A. Edmonds, and A.S. Ward (in review), The influence of floodplain channel connectivity on flood hydrodynamics.|
|This resource is referenced by||Sumaiya, S., J.A. Czuba, J.T. Schubert, S.R. David, G.H. Johnston, and D.A. Edmonds (in review), Sediment transport potential in a hydraulically connected river and floodplain-channel system|
|The content of this resource is derived from||https://www.hydroshare.org/resource/06f7b877a44e45d4973643f9c856c3da/|
|Title||Owners||Sharing Status||My Permission|
|East Fork White River near Seymour, IN||Jonathan Czuba||Public & Shareable||Open Access|
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This resource is shared under the Creative Commons Attribution CC BY.http://creativecommons.org/licenses/by/4.0/
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