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|Created:||Nov 12, 2020 at 3:15 a.m.|
|Last updated:|| Nov 12, 2020 at 3:30 p.m.
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2D HEC-RAS simulated depths 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
Overview of Flows.xlsx -- provides an overview of all 21 steady-state flows simulated in the model with an index value (1-21), the discharge at the USGS Seymour gage, and the "date" of the model simulation result.
> This folder contains TIF files of the exported depth results from HEC-RAS. The date of the file name corresponds to the flows specified in the Excel spreadsheet.
EFWR_FPCN_digi_diss_split.shp -- is a hand-digitized network of connected flow paths created at each successive level of inundation. The attribute "Active" describes the flow (index 1-21) when that "channel" or connected pathway becomes first activated.
|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|
|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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