Continental Hydrologic Intercomparison Project, Phase 1: A Large-Scale Hydrologic Model Comparison Over the Continental United States
| dc.contributor.author | Tijerina, D. | |
| dc.contributor.author | Condon, L. | |
| dc.contributor.author | FitzGerald, K. | |
| dc.contributor.author | Dugger, A. | |
| dc.contributor.author | O’Neill, M.M. | |
| dc.contributor.author | Sampson, K. | |
| dc.contributor.author | Gochis, D. | |
| dc.contributor.author | Maxwell, R. | |
| dc.date.accessioned | 2021-09-03T01:15:13Z | |
| dc.date.available | 2021-09-03T01:15:13Z | |
| dc.date.issued | 2021 | |
| dc.identifier.citation | Tijerina, D., Condon, L., FitzGerald, K., Dugger, A., O’Neill, M. M., Sampson, K., Gochis, D., & Maxwell, R. (2021). Continental Hydrologic Intercomparison Project, Phase 1: A Large-Scale Hydrologic Model Comparison Over the Continental United States. Water Resources Research, 57(7). | |
| dc.identifier.issn | 0043-1397 | |
| dc.identifier.doi | 10.1029/2020WR028931 | |
| dc.identifier.uri | http://hdl.handle.net/10150/661368 | |
| dc.description.abstract | High-resolution, coupled, process-based hydrology models, in which subsurface, land-surface, and energy budget processes are represented, have been applied at the basin-scale to ask a wide range of water science questions. Recently, these models have been developed at continental scales with applications in operational flood forecasting, hydrologic prediction, and process representation. As use of large-scale model configurations increases, it is exceedingly important to have a common method for performance evaluation and validation, particularly given challenges associated with accurately representing large domains. Here, we present phase 1 of a comparison project for continental-scale, high-resolution, processed-based hydrologic models entitled the Continental Hydrologic Intercomparison Project (CHIP). The first phase of CHIP is based on past Earth System Model intercomparisons and comprised of a two-model proof of concept comparing the ParFlow-CONUS hydrologic model, version 1.0 and a NOAA US National Water Model configuration of WRF-Hydro, version 1.2. The objectives of CHIP phase 1 are: (a) describe model physics and components, (b) design an experiment to ensure a fair comparison, and (b) assess simulated streamflow with observations to better understand model bias. To our knowledge, this is the first comparison of continental-scale, high-resolution, physics-based models which incorporate lateral subsurface flow. This model intercomparison is an initial step toward a continued effort to unravel process, parameter, and formulation differences in current large-scale hydrologic models and to engage the hydrology community in improving hydrology model configuration and process representation. © 2021. The Authors. | |
| dc.language.iso | en | |
| dc.publisher | John Wiley and Sons Inc | |
| dc.rights | Copyright © 2021. The Authors. This is an open access article under the terms of the Creative Commons Attribution-NonCommercial License. | |
| dc.rights.uri | https://creativecommons.org/licenses/by-nc/4.0/ | |
| dc.subject | continental-scale model | |
| dc.subject | hydrologic modeling | |
| dc.subject | integrated model | |
| dc.subject | model intercomparison | |
| dc.subject | streamflow | |
| dc.title | Continental Hydrologic Intercomparison Project, Phase 1: A Large-Scale Hydrologic Model Comparison Over the Continental United States | |
| dc.type | Article | |
| dc.type | text | |
| dc.contributor.department | University of Arizona | |
| dc.identifier.journal | Water Resources Research | |
| dc.description.note | Open access article | |
| dc.description.collectioninformation | This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu. | |
| dc.eprint.version | Final published version | |
| dc.source.journaltitle | Water Resources Research | |
| refterms.dateFOA | 2021-09-03T01:15:13Z |

