Articles | Volume 26, issue 3
https://doi.org/10.5194/hess-26-589-2022
https://doi.org/10.5194/hess-26-589-2022
Research article
 | 
07 Feb 2022
Research article |  | 07 Feb 2022

Drivers of drought-induced shifts in the water balance through a Budyko approach

Tessa Maurer, Francesco Avanzi, Steven D. Glaser, and Roger C. Bales

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Cited articles

Abatzoglou, J. T., Redmond, K. T., and Edwards, L. M.: Classification of regional climate variability in the state of California, J. Appl. Meteorol. Clim., 48, 1527–1541, https://doi.org/10.1175/2009JAMC2062.1, 2009. a
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Alvarez-Garreton, C., Pablo Boisier, J., Garreaud, R., Seibert, J., and Vis, M.: Progressive water deficits during multiyear droughts in basins with long hydrological memory in Chile, Hydrol. Earth Syst. Sci., 25, 429–446, https://doi.org/10.5194/hess-25-429-2021, 2021. a
Avanzi, F., Rungee, J., Maurer, T., Bales, R., Ma, Q., Glaser, S., and Conklin, M.: Climate elasticity of evapotranspiration shifts the water balance of Mediterranean climates during multi-year droughts, Hydrol. Earth Syst. Sci., 24, 4317–4337, https://doi.org/10.5194/hess-24-4317-2020, 2020. a, b, c, d, e, f, g, h, i, j, k, l, m, n, o, p, q, r, s, t
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Short summary
Predicting how much water will end up in rivers is more difficult during droughts because the relationship between precipitation and streamflow can change in unexpected ways. We differentiate between changes that are predictable based on the weather patterns and those harder to predict because they depend on the land and vegetation of a particular region. This work helps clarify why models are less accurate during droughts and helps predict how much water will be available for human use.
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