Past aquifer responses to climate recorded by fossil groundwater

Billions of people rely upon groundwater for drinking water and agriculture, yet predicting how climate change may affect aquifer storage remains challenging. To gain insight beyond the short historical record, we reconstruct changes in groundwater levels in western North America during the last glacial termination (LGT, ~20 to 11 thousand years ago) using noble gas isotopes. Our reconstructions indicate remarkable stability of water table depth in a Pacific Northwest aquifer throughout the LGT despite increasing precipitation, closely matching independent Earth system model (ESM) simulations. In the American Southwest, ESM simulations and noble gas isotopes both suggest a pronounced LGT decline in water table depth in in response to decreasing precipitation, indicating distinct regional groundwater responses to climate. Despite the hydrologic simplicity of ESMs, their agreement with proxy reconstructions of past water table depth suggests that these models hold value in understanding groundwater dynamics and projecting large-scale aquifer responses to climate forcing.

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Publication Details

Journal
Science Advances
Published
2025-06-11
DOI
https://doi.org/10.1126/sciadv.adu7812
Citations
1
Primary Topic
Groundwater and Isotope Geochemistry
Type
article
Field-Weighted Citation Impact
1.34
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article

Past aquifer responses to climate recorded by fossil groundwater

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1 citations
Science Advances
Groundwater and Isotope Geochemistry
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article

Past aquifer responses to climate recorded by fossil groundwater

Rebecca Tyne, Kristopher B. Karnauskas, William J. Jenkins, Jeff B. Langman, Michael W. Broadley, Dillon J. Amaya, Peter H. Barry, Gabriel J. Bowen, Juan M. Lora, David V. Bekaert, Maya Costantini, Alan Seltzer, Israela Musan
article en
1 citations

Abstract

Billions of people rely upon groundwater for drinking water and agriculture, yet predicting how climate change may affect aquifer storage remains challenging. To gain insight beyond the short historical record, we reconstruct changes in groundwater levels in western North America during the last glacial termination (LGT, ~20 to 11 thousand years ago) using noble gas isotopes. Our reconstructions indicate remarkable stability of water table depth in a Pacific Northwest aquifer throughout the LGT despite increasing precipitation, closely matching independent Earth system model (ESM) simulations. In the American Southwest, ESM simulations and noble gas isotopes both suggest a pronounced LGT decline in water table depth in in response to decreasing precipitation, indicating distinct regional groundwater responses to climate. Despite the hydrologic simplicity of ESMs, their agreement with proxy reconstructions of past water table depth suggests that these models hold value in understanding groundwater dynamics and projecting large-scale aquifer responses to climate forcing.

Science AdvancesVol. 11(24)
Planetary Science Institute (US), National Oceanic and Atmospheric Administration (US), University of Idaho (US), Cooperative Institute for Research in Environmental Sciences (US), University of Colorado Boulder (US), University of Utah (US), University of Manchester (GB), Yale University (US), Centre National de Recherches Météorologiques (FR), Centre de Recherches Pétrographiques et Géochimiques (FR), NOAA Physical Sciences Laboratory (US), Woods Hole Oceanographic Institution (US)
Openalex Percentile: Top 19%
Groundwater and Isotope Geochemistry
1.34
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