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• W2895413567 abstract "Significance Across the world, the seasonal montane snowpack stores and releases substantial amounts of water annually. As the global temperature is projected to rise, it becomes increasingly important to assess the vulnerability of the mountain snowpack. We therefore turn to the historical record to understand the extent to which snow water equivalent (SWE) and its centroid respond to different levels of warming. Using a probabilistic framework, we show that even a 1.0 or 2.0 °C increase in average temperature leads to approximately a 20 to 40% increase in the likelihood of below average SWE. We also quantify changes in the distribution of the amount of SWE and where it is stored elevationally across the mountain range given warmer winters." @default.
• W2895413567 created "2018-10-12" @default.
• W2895413567 creator A5050684806 @default.
• W2895413567 creator A5072264931 @default.
• W2895413567 date "2018-10-08" @default.
• W2895413567 modified "2023-09-25" @default.
• W2895413567 title "Mountain snowpack response to different levels of warming" @default.
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• W2895413567 doi "https://doi.org/10.1073/pnas.1805953115" @default.
• W2895413567 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/6205460" @default.
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• W2895413567 hasPublicationYear "2018" @default.
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