Wind and topography underlie correlation between seasonal snowpack, mountain glaciers, and late-summer streamflow
<p>In a warming climate, net mass loss from perennial snow and ice (PSI) contributes a temporary source of unsustainable streamflow. However, the role of topography and wind in mediating the streamflow patterns of deglaciating watersheds is unknown. We compare lidar surveys of seasonal snow an...
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| Main Authors: | , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2025-08-01
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| Series: | The Cryosphere |
| Online Access: | https://tc.copernicus.org/articles/19/3193/2025/tc-19-3193-2025.pdf |
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