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• W4313639945 abstract "The mountainous regions across the globe face consistent soil erosion and pose a significant cause for land degradation. This present study estimates the soil loss rate variation on the basin-scale due to an Extreme Hydrological Event (EHE). On 3rd August 2012, an EHE changed the geomorphology and landcover of the Assiganga River basin which lies in the northwest Himalaya (the third pole region) and deposited a large volume of sediments in its several reaches. The EHE also increased the sediment bar areas from 70 × 10 3 m 2 to 89 × 10 3 m 2 in the lower reaches of the Assiganga River and thus influenced the soil erosion rate. Multi-temporal spatial data integrated with the Google Earth Engine (GEE) and Geographical Information System (GIS) techniques are used in the RUSLE model to estimate the pre-post event monthly soil erosion rate. Crop management (C) and support practice (P) factors are calculated by assigning appropriate values to the LULC classes derived from the supervised classification of Landsat-7 images in the GEE platform using the Classification And Regression Tree (CART) classifier. The Rainfall erosivity (R), Soil erodibility (K), and Slope length and steepness (LS) factors are derived from the Center for Hydrometeorology and Remote Sensing (CHRS), National Bureau of Soil Survey and Land Use Planning (NBSS-LUP) soil texture maps, and the ALOS-PALSAR Digital Elevation Model (DEM), respectively, in the GIS environment. The results reveal that the average soil loss rate in the Assiganag River basin has increased from 2.64 tons/ha/month in May 2012 (pre-event) to 3.35 tons/ha/month in October 2012 (post-event), even with less rainfall. The significant increase in soil erosion rate observed in sandy areas from 11.35 tons/ha/month to 13.31 tons/ha/month suggests that an extreme hydrological event can significantly alter the geomorphology and thereby influence the rate of soil loss." @default.
• W4313639945 created "2023-01-07" @default.
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• W4313639945 date "2022-12-10" @default.
• W4313639945 modified "2023-10-10" @default.
• W4313639945 title "Extreme Hydrological Event‐Induced Temporal Variation in Soil Erosion of the Assiganga River Basin, <scp>NW</scp> Himalaya" @default.
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• W4313639945 doi "https://doi.org/10.1002/9781119787754.ch15" @default.
• W4313639945 hasPublicationYear "2022" @default.
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