Topography and flow model files for the Platte River, Nebraska, 2016-2017
2017-10-13
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View StatisticsCollection period
2016-06-01
2017-05-31
2017-05-31
Date completed
2017-10-10
Date updated
Time period coverage
Geographic coverage
-99.52 -99.39 40.67 40.69
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Title
Topography and flow model files for the Platte River, Nebraska, 2016-2017
Published Date
2017-10-13
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Limaye, Ajay B
aslimaye@umn.edu
aslimaye@umn.edu
Type
Dataset
Simulation Data
Spatial Data
Simulation Data
Spatial Data
Abstract
Automated techniques for extracting channels from topography are well developed for convergent channel networks, and identify flow paths based on land-surface gradients. These techniques—even when they allow multiple flow paths—do not consistently capture channel networks with frequent bifurcations (e.g., in rivers, deltas, and alluvial fans). The project uses multithread rivers as a template to develop a new approach for channel extraction suitable for channel networks with divergences. This data set includes topography and flow model data used to demonstrate this new approach for automated identification of channels on planetary surfaces. The data set accompanies a 2017 publication in the Journal of Geophysical Research: Earth Surface.
Description
The data set includes raw and processed data for a digital elevation model; files for executing an open-source flow model; and maps of flow depth produced by this model.
Referenced by
Limaye A. B. (2017). Extraction of multithread channel networks with a reduced-complexity flow model. Journal of Geophysical Research: Earth Surface, 122.
https://doi.org/10.1002/2016JF004175
https://doi.org/10.1002/2016JF004175
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Funding information
St. Anthony Falls Laboratory Industrial Consortium
National Center for Earth-surface Dynamics 2
National Center for Earth-surface Dynamics 2
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Suggested citation
Limaye, Ajay B. (2017). Topography and flow model files for the Platte River, Nebraska, 2016-2017. Retrieved from the Data Repository for the University of Minnesota (DRUM), https://doi.org/10.13020/D6Z39J.
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