Debris flow initiation by runoff in a recently burned basin: Is grain‐by‐grain sediment bulking or en masse failure to blame?
Postwildfire debris flows are frequently triggered by runoff following high‐intensity rainfall, but the physical mechanisms by which water‐dominated flows transition to debris flows are poorly understood relative to debris flow initiation from shallow landslides. In this study, we combined a numeric...
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Veröffentlicht in: | Geophysical research letters 2017-07, Vol.44 (14), p.7310-7319 |
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Sprache: | eng |
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