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Energy‐Water Asynchrony Principally Determines Water Available for Runoff From Snowmelt in Continental Montane Forests


Abstract Changes in the volume, rate, and timing of the snowmelt water pulse have profound implications for seasonal soil moisture, evapotranspiration (ET), groundwater recharge, and downstream water availability, especially in the context of climate change. Here, we present an empirical analysis of water available for runoff using five eddy covariance towers located in continental montane forests across a regional gradient of snow depth, precipitation seasonality, and aridity. We specifically investigated how energy‐water asynchrony (i.e., snowmelt timing relative to atmospheric demand), surface water input intensity (rain and snowmelt), and observed winter ET (winter AET) impact multiple water balance metrics that determine water available for runoff (WAfR). Overall, we found that WAfR had the strongest relationship with energy‐water asynchrony (adjusted r 2 = 0.52) and that winter AET was correlated to total water year evapotranspiration but not to other water balance metrics. Stepwise regression analysis demonstrated that none of the tested mechanisms were strongly related to the Budyko‐type runoff anomaly (highest adjusted r 2 = 0.21). We, therefore, conclude that WAfR from continental montane forests is most sensitive to the degree of energy‐water asynchrony that occurs. The results of this empirical study identify the physical mechanisms driving variability of WAfR in continental montane forests and are thus broadly relevant to the hydrologic management and modelling communities.
Authors Ryan Webb University of WyomingORCID , John F. Knowles ORCID , A. K. Fox University of Wyoming , Alex Fabricus University of Wyoming , Timothy D. Corrie University of Wyoming , Kori Mooney University of Wyoming , Jocelyn Gallais University of Wyoming , Nana Afua Gyau Frimpong University of Wyoming , Christopher A. Akurugu University of Wyoming , G. Barron-Gafford ORCID , Peter D. Blanken ORCID , Sean P. Burns ORCID , J. M. Frank ORCID , M. E. Litvak ORCID
Journal Info Wiley | Hydrological Processes , vol: 38 , iss: 10
Publication Date 10/8/2024
ISSN 0885-6087
TypeKeyword Image article
Open Access hybrid Hybrid Access
DOI https://doi.org/10.1002/hyp.15297
KeywordsKeyword Image Snowmelt (Score: 0.9117212) , Water balance (Score: 0.60864085) , Meltwater (Score: 0.43573433)