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The role of groundwater in contributing to surface water salinization in the Upper Colorado River Basin

Matthew P. Miller·Olivia L. Miller·Patrick C. Longley·Daniel R. Wise·Morgan C. McDonnell·Noah M. Schmadel·Jay R. Alder
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Abstract

Freshwater salinization impacts the availability of water for human use and ecosystem needs worldwide. It has been estimated that total dissolved solids (TDS) in the Colorado River Basin cause $350 million/year in damages and substantial resources are devoted to reducing TDS loading to streams. This study describes the development and application of coupled watershed models that enable TDS source tracking through the subsurface and across the landscape at a seasonal timestep for 35 years in the Upper Colorado River Basin. Results indicate that, on average, 75% of TDS loading to streams originates as baseflow, and 50% of loading is lagged in delivery by longer than one season. Snowmelt was identified as a dominant process controlling the transport of lagged TDS to streams. This approach informs when and where TDS mitigation efforts may be effective in a watershed that serves as a critical water supply for the southwestern United States.

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Geophysical Research LettersArticle
90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 36.020335240877046° to 42.82938512458236° latitude; -110.90060995927905° to -107.09503766746343° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeXRIS

Matthew P. Miller, Olivia L. Miller, Patrick C. Longley, Daniel R. Wise, Morgan C. McDonnell, Noah M. Schmadel, Jay R. Alder. 2026-04-18. The role of groundwater in contributing to surface water salinization in the Upper Colorado River Basin. https://doi.org/10.1029/2025gl118834

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United STates placeUpper Colorado River Basin placeArizona, Colorado, New Mexico, Utah, Wyoming placeArticle subjectGeophysical Research Letters subject

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