Abstract
Reconstructed historical streamflow time series can supplement limited streamflow gauge observations. However, there are common challenges of typical modeling approaches: process-based hydrologic models can be data/computation-intensive, and statistics-based models can be region/stream-specific. Here we present a nationally scalable modeling framework integrating the simulated runoff from the Variable Infiltration Capacity (VIC) model with the Routing Application for Parallel computatIon of Discharge (RAPID) routing model leveraging high-performance computing. We demonstrate an efficient method of assimilating streamflow at US Geological Survey (USGS) streamflow monitoring sites using a simple hierarchical approach in the VIC-RAPID framework. The result is a reconstructed 36-year (1980–2015) daily and monthly streamflow dataset (Dayflow) at ∼2.7 million NHDPlusV2 stream reaches in the conterminous US (CONUS). We perform a comprehensive evaluation at 7,526 USGS sites and characterize their error statistics. The results demonstrate that 49% of the USGS sites demonstrate Kling–Gupta Efficiency (KGE) > 0.5 and 58% of the sites show percentage bias within ±20% for the daily naturalized streamflow. Streamflow data assimilation across CONUS shows an overall improvement over naturalized streamflow, notably in the western semiarid-to-arid regions. Comparison to other national and global streamflow reanalysis datasets such as the National Water Model and Global Reach-scale A priori Discharge Estimates for SWOT demonstrates improved KGE, reduced bias, and directions for Dayflow improvements. Investigations of error statistics with key hydrologic, hydroclimatic, and geomorphologic basin characteristics reveal region-specific patterns which may help improve future framework applications. Overall, Dayflow may enable a better understanding of hydrologic conditions in a changing environment, especially in locations currently not represented by streamflow monitoring networks.
Original language | English |
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Article number | e2022WR032312 |
Journal | Water Resources Research |
Volume | 59 |
Issue number | 2 |
DOIs | |
State | Published - Feb 2023 |
Funding
This study is supported by the USGS. Department of Energy (DOE) Water Power Technologies Office. The research used resources of the Oak Ridge Leadership Computing Facility at Oak Ridge National Laboratory, which is a DOE Office of Science User Facility. PET was supported as part of the Energy Exascale Earth System Model (E3SM) project, funded by the US DOE, Office of Science, Office of Biological and Environmental Research. The authors are employees of UT‐Battelle, LLC, under contract DE‐AC05‐00OR22725 with the US DOE. Accordingly, the US government retains and the publisher, by accepting the article for publication, acknowledges that the US government retains a nonexclusive, paid‐up, irrevocable, worldwide license to publish or reproduce the published form of this manuscript or allow others to do so, for US Government purposes. This study is supported by the USGS. Department of Energy (DOE) Water Power Technologies Office. The research used resources of the Oak Ridge Leadership Computing Facility at Oak Ridge National Laboratory, which is a DOE Office of Science User Facility. PET was supported as part of the Energy Exascale Earth System Model (E3SM) project, funded by the US DOE, Office of Science, Office of Biological and Environmental Research. The authors are employees of UT-Battelle, LLC, under contract DE-AC05-00OR22725 with the US DOE. Accordingly, the US government retains and the publisher, by accepting the article for publication, acknowledges that the US government retains a nonexclusive, paid-up, irrevocable, worldwide license to publish or reproduce the published form of this manuscript or allow others to do so, for US Government purposes.
Keywords
- Dayflow
- GRADES
- RAPID
- VIC
- national water model
- streamflow reanalysis
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CMIP6-based Multi-model Streamflow Projections over the Conterminous US
Kao, S.-C. (Creator), Ghimire, G. (Creator) & Gangrade, S. (Creator), HydroSource, Oct 1 2023
DOI: 10.21951/9505V3Flow/2007926
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