The importance of explicitly representing the streambed in watershed models

Journal Article · 17 December 2023 · Hydrological Processes

DOI: https://doi.org/10.1002/hyp.15043 · OSTI ID:2242547

Shuai, Pin  ^[1]; Jiang, Peishi ^[2]; Coon, Ethan T. ^[3]; Chen, Xingyuan ^[2]

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1. Utah State Univ., Logan, UT (United States); Pacific Northwest National Laboratory (PNNL), Richland, WA (United States)
2. Pacific Northwest National Laboratory (PNNL), Richland, WA (United States)
3. Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)

The streambed is the critical interface between the aquatic and terrestrial systems and hosts important biogeochemical hot spots within river corridors. Although the streambed characteristics are significantly different from those of its surrounding soil, the streambed itself has not been explicitly represented in watershed models. Here, we explicitly incorporated a streambed layer into an integrated hydrologic model through model parameterization and discretization. We examined the hydrological effects of streambed characteristics, including hydraulic conductivity (K), layer thickness, and resolution, on the exchange fluxes across the streambed as well as the streamflow at the watershed outlet. The numerical experiments were performed in the American River Watershed, a headwater, mountainous watershed within the Yakima River Basin in central Washington. Despite having a negligible effect on the watershed streamflow, an explicit representation of the streambed with distinctive properties dramatically changed the magnitude and variability of the exchange flux. In general, a larger streambed K along with a thicker streambed layer induced larger exchange fluxes. The exchange flux was most sensitive to the streambed resolution. A finer streambed resolution increased exchange fluxes per unit area while reducing the overall exchange volumes across the entire streambed. The amount of baseflow decreased by 6% as the streambed resolution increased from 250 to 50 m. This finding is important because these hydrological changes may, in turn, affect the exchange of nutrients and contaminants between surface water and groundwater and the associated biogeochemical processes. Our work demonstrated the importance of representing streambeds in fully distributed, process-based watershed models to better capture the exchange flow dynamics in river corridors.

• Research Organization: Pacific Northwest National Laboratory (PNNL), Richland, WA (United States); Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States). National Energy Research Scientific Computing Center (NERSC)
• Sponsoring Organization: USDOE Office of Science (SC), Biological and Environmental Research (BER); USDOE
• Grant/Contract Number: AC05-76RL01830; AC02-05CH11231
• OSTI ID: 2242547
• Alternate ID(s): OSTI ID: 2263279; OSTI ID: 2263346
• Report Number(s): PNNL-SA-184264
• Journal Information: Hydrological Processes, Vol. 37, Issue 12; ISSN 0885-6087
• Publisher: WileyCopyright Statement
• Country of Publication: United States
• Language: English