James Buttle Review: Dynamic Water Storage Shapes Critical Zone Function in Snow‐Dominated Mountain Watersheds

ABSTRACT Dynamic water storage is the water that remains for enough time in watersheds to influence streamflow generation, chemically weather rock and drive the release of solutes, breakdown organic carbon (C) through microbial activity, and sustain vegetation between periods of precipitation. The amount and connectivity of dynamic water stores control critical zone processes, including evapotranspiration, vegetation productivity and mortality, streamflow, weathering and solute transport. Here, we present recent advances and identify frontiers in the study of dynamic water storage in the critical zone, focusing on observational techniques for quantifying dynamic storage, advances in conceptual and numerical models that capture dynamic storage, and emerging hypotheses that drive dynamic storage evolution. We specifically identify and focus on four primary dynamic water storages: snow, plant‐accessible water, groundwater, and surface water. While we use semi‐arid mountain environments as an exemplar of dynamic storage controls on critical zone processes, this work offers implications for a broad range of geoclimatic settings.

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Publication Details

Journal
Hydrological Processes
Published
2025-11-01
DOI
https://doi.org/10.1002/hyp.70325
Citations
1
Primary Topic
Hydrology and Watershed Management Studies
Type
article
Field-Weighted Citation Impact
0.82

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article

James Buttle Review: Dynamic Water Storage Shapes Critical Zone Function in Snow‐Dominated Mountain Watersheds

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James Buttle Review: Dynamic Water Storage Shapes Critical Zone Function in Snow‐Dominated Mountain Watersheds

Holly Barnard, C. Heckman, Katherine B. Lininger, Keira Johnson, A. A. Harpold, John F. Knowles, Lauren E. L. Lowman, Alexis Navarre‐Sitchler, Eric Parrish, C. Tague, Kamini Singha, Sara R. Warix, Pamela Sullivan
article en
1 citations

Abstract

ABSTRACT Dynamic water storage is the water that remains for enough time in watersheds to influence streamflow generation, chemically weather rock and drive the release of solutes, breakdown organic carbon (C) through microbial activity, and sustain vegetation between periods of precipitation. The amount and connectivity of dynamic water stores control critical zone processes, including evapotranspiration, vegetation productivity and mortality, streamflow, weathering and solute transport. Here, we present recent advances and identify frontiers in the study of dynamic water storage in the critical zone, focusing on observational techniques for quantifying dynamic storage, advances in conceptual and numerical models that capture dynamic storage, and emerging hypotheses that drive dynamic storage evolution. We specifically identify and focus on four primary dynamic water storages: snow, plant‐accessible water, groundwater, and surface water. While we use semi‐arid mountain environments as an exemplar of dynamic storage controls on critical zone processes, this work offers implications for a broad range of geoclimatic settings.

Hydrological ProcessesVol. 39(11)
Oregon State University (US), University of Nevada, Reno (US), University of California, Santa Barbara (US), Colorado School of Mines (US), Institute of Arctic and Alpine Research (US), University of Colorado Boulder (US), University of Utah (US), Montana State University (US), Virginia Tech - Wake Forest University School of Biomedical Engineering & Sciences (US), Louisiana Department of Natural Resources (US), Wake Forest University (US), University of Montana (US)
National Science Foundation
Openalex Percentile: Top 21%
Hydrology and Watershed Management Studies
0.82
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