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Geomorphic changes and sediment yield dynamics in Alpine hillslopes: the role of surface temperature and rainfall intensity
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DOI:10.1016/j.catena.2026.110489.png)
Abstract
En 中文
• Marked soil loss observed from an avalanche-affected experimental hillslope. • Freeze-thaw cycles strongly influence hillslope soil erosion in the Alps. • Sediment yield correlates positively with both temperature and rainfall intensity.
Keywords:
Sediment yield
Alpine hillslope
Erosion
Geomorphological changes
Meteorological forcing
Avalanches
Journal
IF:
5.7
Papers:
9.2K
Citations:
3.8W
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