Understanding hydrogeomorphic and climatic controls on soil erosion and sediment dynamics in large Himalayan basins

The Himalayan basins are characterised by severe soil erosion rates and several basins are among the largest sediment dispersal systems in the world. Unsustainable agricultural activities increase the soil erosion rates and influence the overall hydro-geomorphic regime of river basins. Consequently, the water holding capacity of soil reduces, which enhances the flood risk in the lowland regions. In addition, excessive sediment flux severely affects the reservoir capacity in the mountainous regions, thus amplifying the flood hazard in the upland regions. Here, we have analysed two large and hydro-geomorphically diverse Himalayan River basins, namely, the Ganga Basin (GBA) from source to Allahabad in northern India and the Kosi Basin (KB) draining through Nepal and north Bihar plains in eastern India. Based on RULSE and region-specific SDR modelling framework, which includes model calibration, validation and uncertainty assessment, we demonstrate that spatial variation in rainfall, hydrogeomorphic conditions, the presence of hydraulic structures, and large-scale agricultural activities influence the overall pattern of sediment production and transport in these two large river basins. Total soil erosion in GBA and KB are estimated to be similar to 404 x 10(6) t/y and similar to 724 x 10(6) t/y respectively, a large part of which comes from the mountainous regions in both basins. Sediment yield at the mountain exits of the GBA and KB are computed as 14.1 x 10(6) t/y and 86.4 x 10(6) t/y respectively, which work out to be similar to 5% and similar to 15% of total soil erosion from the respective contributing areas of the KB and GBA respectively. Similarly, sediment yields at outlets in the alluvial plains are estimated to be 32.2 x 10(6) t/y and 37.3 x 10(6) t/y in the GBA and the KB, respectively suggesting that a large part of sediments are accommodated in the alluvial plains of KB. These results have significant implications for sediment management in the Himalayan River basins. (C) 2021 Elsevier B.V. All rights reserved.

Automated summary

The Himalayan basins are characterized by severe soil erosion rates, which are exacerbated by unsustainable agricultural activities, impacting the overall hydro-geomorphic regime of river basins. Research findings demonstrate that a significant portion of sediment production in the Ganga and Kosi basins comes from the mountainous regions, with a large proportion of sediment accommodation in the alluvial plains of the Kosi Basin.