Predicting Changes in Hillslope Freeze–Thaw Potential Due To Climate Change
Abstract Freeze‐thaw (FT) is a key hillslope weathering process in cold regions, influencing hillslope stability and sediment delivery to rivers. To understand how climate change will impact FT, we conducted field monitoring in the Pekerebetsu River basin, Hokkaido, Japan, and calibrated a numerical...
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| Format: | Artigo |
| Sprache: | Inglês |
| Veröffentlicht: |
Wiley
2025-10-01
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| Schriftenreihe: | AGU Advances |
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| Online-Zugang: | https://doi.org/10.1029/2025AV001810 |
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