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| Type: | Resource | |
| Storage: | The size of this resource is 1.3 GB | |
| Created: | Aug 12, 2020 at 10:11 p.m. | |
| Last updated: | Oct 06, 2020 at 2:15 p.m. (Metadata update) | |
| Published date: | Oct 06, 2020 at 2:15 p.m. | |
| DOI: | 10.4211/hs.172bf3533b1d46ea8d89feea51d44fb7 | |
| Citation: | See how to cite this resource |
| Sharing Status: | Published |
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| Views: | 1548 |
| Downloads: | 52 |
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Abstract
This resource is a modified version of the Hillslope River Routing (HRR) model (Beighley et al., 2009), which now derives surface and subsurface flow using the Variable Infiltration Capacity (VIC) model formulation equations (Liang et al., 1994), termed the HRR-VIC model. HRR is a topography-based routing model that integrates surface and subsurface runoff laterally into river channels and routes discharges throughout the river network based on the Muskingum–Cunge method, resulting in discharge estimates for each river reach. Model results and code for 39 gauges in the Ohio River Basin over a 9 year span is presented, as a reference for the study, "The Applicability of SWOT’s Non-Uniform Space–Time Sampling in Hydrologic Model Calibration," doi:10.3390/rs12193241.
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| This resource is referenced by | Nickles, C., Beighley, E., & Feng, D. (2020). The Applicability of SWOT’s Non-Uniform Space–Time Sampling in Hydrologic Model Calibration. Remote Sensing, 12(19), 3241. doi:10.3390/rs12193241 |
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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