Extreme Snowfall at High Elevations: A Historical Analysis of Elevation-Dependent SWE Trends in a Warming Climate
Warming temperatures are causing an uphill shift of the rain-snow transition zone, reducing snow at lower elevations. However, a warmer atmosphere can retain and transport more moisture, increasing the chance of extreme precipitation events. We hypoth
Authors
- Seong-Su Ryu (ORCID: https://orcid.org/0000-0001-7567-8404)
- Manuela Girotto (ORCID: https://orcid.org/0000-0003-2795-2063)
- Stefano Casirati (ORCID: https://orcid.org/0009-0002-1508-7869)
Institutions
- University of California, Berkeley (US)
Publication Details
- Published
- 2025-10-13
- DOI
- https://doi.org/10.22541/essoar.176036960.01383911/v1
- Primary Topic
- Meteorological Phenomena and Simulations
- Type
- article
- Field-Weighted Citation Impact
- 0.00