Isotopic evaluation of the National Water Model reveals missing agricultural irrigation contributions to streamflow across the western United States

Hydrology and Earth Systems Science
By: , and 

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Abstract

The National Water Model (NWM) provides critical analyses and projections of streamflow that support water management decisions. However, the NWM performs poorly in lower-elevation rivers of the western United States (US). The accuracy of the NWM depends on the fidelity of the model inputs and the representation and calibration of model processes and water sources. To evaluate the NWM performance in the western US, we compared observations of river water isotope ratios (18O 16O and 2H 1H expressed in δ notation) to NWM-flux-estimated (model) river reach isotope ratios. The modeled estimates were calculated from long-term (2000–2019) mean summer (June, July, and August) NWM hydrologic fluxes and gridded isotope ratios using a mass balance approach. The observational dataset comprised 4503 in-stream water isotope observations in 877 reaches across 5 basins. A simple regression between observed and modeled isotope ratios explained 57.9 % (δ18O) and 67.1 % (δ2H) of variance, although observations were 0.5 ‰ (δ18O) and 4.8 ‰ (δ2H) higher, on average, than mass balance estimates. The unexplained variance suggest that the NWM does not include all relevant water fluxes to rivers. To infer possible missing water fluxes, we evaluated patterns in observation–model differences using δ18Odiff (δ18Oobsδ18Omod) and ddiff (). We detected evidence of evaporation in observations but not model estimates (negative ddiff and positive δ18Odiff) at lower-elevation, higher-stream-order, arid sites. The catchment actual-evaporation-to-precipitation ratio, the fraction of streamflow estimated to be derived from agricultural irrigation, and whether a site was reservoir-affected were all significant predictors of ddiff in a linear mixed-effects model, with up to 15.2 % of variance explained by fixed effects. This finding is supported by seasonal patterns, groundwater levels, and isotope ratios, and it suggests the importance of including irrigation return flows to rivers, especially in lower-elevation, higher-stream-order, arid rivers of the western US.

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Publication type Article
Publication Subtype Journal Article
Title Isotopic evaluation of the National Water Model reveals missing agricultural irrigation contributions to streamflow across the western United States
Series title Hydrology and Earth Systems Science
DOI 10.5194/hess-28-2895-2024
Volume 28
Issue 13
Year Published 2024
Language English
Publisher European Geosciences Union
Contributing office(s) New York Water Science Center, Utah Water Science Center
Description 24 p.
First page 2895
Last page 2918
Country United States
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