[HTML][HTML] Towards the assessment of sediment connectivity in a large Himalayan river basin
Sediment connectivity, defined as the degree of linkage between the sediment sources to
downstream areas, is one of the most important properties that control landscape evolution
in river basins. The degree of linkages amongst different parts of a catchment depends
mainly on the hinterland characteristics (eg catchment morphology, slope, shape, relief, and
elevation), channel characteristics (eg slope, stream network density, valley confinement),
and the combined effects of vegetation (eg land use changes and land abandonment). This …
downstream areas, is one of the most important properties that control landscape evolution
in river basins. The degree of linkages amongst different parts of a catchment depends
mainly on the hinterland characteristics (eg catchment morphology, slope, shape, relief, and
elevation), channel characteristics (eg slope, stream network density, valley confinement),
and the combined effects of vegetation (eg land use changes and land abandonment). This …
Towards the assessment of sediment connectivity in a large Himalayan river basin.
KM Kanchan Mishra, RS Rajiv Sinha, VJ Vikrant Jain… - 2019 - cabidigitallibrary.org
Sediment connectivity, defined as the degree of linkage between the sediment sources to
downstream areas, is one of the most important properties that control landscape evolution
in river basins. The degree of linkages amongst different parts of a catchment depends
mainly on the hinterland characteristics (eg catchment morphology, slope, shape, relief, and
elevation), channel characteristics (eg slope, stream network density, valley confinement),
and the combined effects of vegetation (eg land use changes and land abandonment). This …
downstream areas, is one of the most important properties that control landscape evolution
in river basins. The degree of linkages amongst different parts of a catchment depends
mainly on the hinterland characteristics (eg catchment morphology, slope, shape, relief, and
elevation), channel characteristics (eg slope, stream network density, valley confinement),
and the combined effects of vegetation (eg land use changes and land abandonment). This …
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