Articles | Volume 30, issue 19
https://doi.org/10.5194/hess-30-6131-2026
https://doi.org/10.5194/hess-30-6131-2026
Research article
 | 
01 Oct 2026
Research article |  | 01 Oct 2026

Assessing the seasonal compartmentalization of water fluxes in the soil-plant-atmosphere continuum of a high-elevation mountain grassland

Alessio Gentile, Davide Gisolo, Stefano Brighenti, Giulia Zuecco, Chiara Marchina, Davide Canone, Tanzeel Hamza, Stefano Ferrari, Stefano Bechis, and Stefano Ferraris

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Cited articles

Ajami, H., Meixner, T., Dominguez, F., Hogan, J., and Maddock III, T.: Seasonalizing Mountain System Recharge in Semi-Arid Basins-Climate Change Impacts, Groundwater, 50, 585–597, https://doi.org/10.1111/j.1745-6584.2011.00881.x, 2012. 
Allen, S. T. and Kirchner, J. W.: Potential effects of cryogenic extraction biases on plant water source partitioning inferred from xylem-water isotope ratios, Hydrol. Process., 36, e14483, https://doi.org/10.1002/hyp.14483, 2022. 
Allen, S. T., Kirchner, J. W., Braun, S., Siegwolf, R. T. W., and Goldsmith, G. R.: Seasonal origins of soil water used by trees, Hydrol. Earth Syst. Sci., 23, 1199–1210, https://doi.org/10.5194/hess-23-1199-2019, 2019a. 
Allen, S. T., Freyberg, J. von, Weiler, M., Goldsmith, G. R., and Kirchner, J. W.: The Seasonal Origins of Streamwater in Switzerland, Geophys. Res. Lett., 46, 10425–10434, https://doi.org/10.1029/2019GL084552, 2019b. 
Allen, S. T., Sprenger, M., Bowen, G. J., and Brooks, J. R.: Spatial and Temporal Variations in Plant Source Water: O and H Isotope Ratios from Precipitation to Xylem Water, in: Stable Isotopes in Tree Rings: Inferring Physiological, Climatic and Environmental Responses, edited by: Siegwolf, R. T. W., Brooks, J. R., Roden, J., and Saurer, M., Springer International Publishing, Cham, 501–535, https://doi.org/10.1007/978-3-030-92698-4_18, 2022. 
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Short summary
This study explores how snowmelt and rainfall supply water to plants and groundwater in a high-elevation mountain grassland. Using field data and model simulations, we tracked how snowmelt and summer rain move through the soil. Snowmelt mainly supplies deep drainage, while rain mainly feeds plants. Nevertheless, during a very dry year, snowmelt contributed more than usual to plant water use. These results show how reduced snowfalls and droughts may affect the mountain water cycle.
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