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Particulate forms declined sharply through a reduction in sediment delivery.
Therefore we applied the sediment delivery distributed model which incorporates revised universal soil loss equation (RUSLE) and sediment delivery ratio.
This study highlights the potentials of runoff self-regulation in controlling soil erosion and sediment delivery.
The budget calculations indicate that the study catchment has a sediment delivery ratio of ∼15%.
As the primary sink for sediment delivery, AYRM received approximately 68% of sediment delivery during the study period and sedimentation was mainly occurred in the shallower area where water depth was less than 10 m.
Debris flow volume was calculated with an empirical model, and fine sediment delivery was calculated using simple, expert-based assumptions.
Next, these scenarios were used as an input for a spatially distributed sediment delivery model in order to evaluate their impact on soil erosion and sediment delivery.
Soil retention was calculated using the InVEST sediment delivery ratio model as the average annual amount of soil loss from each parcel of land.
Czuba, J. A. & Foufoula-Georgiou, E. A network-based framework for identifying potential synchronizations and amplifications of sediment delivery in river basins.
We conclude that future acceleration of melt and ice sheet flow may increase sediment delivery from Greenland to its fjords and the nearby ocean.
Therefore, modelled rates of sediment delivery are lower than observed values.
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