From drought to flood: A water balance analysis of the Tuolumne River basin during extreme conditions (2015–2017)
The degree to which the hydrologic water balance in a snow‐dominated headwater catchment is affected by annual climate variations is difficult to quantify, primarily due to uncertainties in measuring precipitation inputs and evapotranspiration (ET) losses. Over a recent three‐year period, the snowpa...
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Veröffentlicht in: | Hydrological processes 2020-05, Vol.34 (11), p.2560-2574, Article hyp.13749 |
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