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- W1640184946 abstract "Abstract Slope disturbances are key sources of sediment, and the impact and recovery of disturbance on downslope erosion is poorly understood. We measured the erosional response of varying extents of slope disturbance in small permafrost catchments for 5 years following disturbance by active layer detachments. Initial erosion rates increased with the size of disturbance, but subsequent fluxes depended on specific morphological evolution of disturbances. Varying degrees of (i) channel density within the disturbances, (ii) downstream channel connectivity, and (iii) geomorphic evolution of disturbances lead to significant differences in catchment response to disturbance. Our results indicate that new equilibrium states of sediment erosion are achieved within the most disturbed and channelized catchments and contribute to greater heterogeneity of erosion on the landscape." @default.
- W1640184946 created "2016-06-24" @default.
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- W1640184946 date "2014-08-01" @default.
- W1640184946 modified "2023-10-10" @default.
- W1640184946 title "Erosion dynamics following localized permafrost slope disturbances" @default.
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- W1640184946 doi "https://doi.org/10.1002/2014gl060677" @default.
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