Continental-scale analysis of shallow and deep groundwater contributions to streams

Nature Communications
By: , and 



Groundwater discharge generates streamflow and influences stream thermal regimes. However, the water quality and thermal buffering capacity of groundwater depends on the aquifer source-depth. Here, we pair multi-year air and stream temperature signals to categorize 1729 sites across the continental United States as having major dam influence, shallow or deep groundwater signatures, or lack of pronounced groundwater (atmospheric) signatures. Approximately 40% of non-dam stream sites have substantial groundwater contributions as indicated by characteristic paired air and stream temperature signal metrics. Streams with shallow groundwater signatures account for half of all groundwater signature sites and show reduced baseflow and a higher proportion of warming trends compared to sites with deep groundwater signatures. These findings align with theory that shallow groundwater is more vulnerable to temperature increase and depletion. Streams with atmospheric signatures tend to drain watersheds with low slope and greater human disturbance, indicating reduced stream-groundwater connectivity in populated valley settings.

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Publication type Article
Publication Subtype Journal Article
Title Continental-scale analysis of shallow and deep groundwater contributions to streams
Series title Nature Communications
DOI 10.1038/s41467-021-21651-0
Volume 12
Year Published 2021
Language English
Publisher Nature
Contributing office(s) Utah Water Science Center, WMA - Earth System Processes Division
Description 1450, 10 p.
Country United States
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