2022
DOI: 10.1002/ldr.4473
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Temporal and spatial variability of suspended sediment rating curves for rivers draining into the Ethiopian Rift Valley

Abstract: Quantification of suspended sediment dynamics is a proxy for the intensity of soil erosion processes in a catchment. However, direct measurement of suspended sediments is difficult. Long-term-based discharge-suspended sediment relationships often fail to provide sufficiently accurate results due to the temporal variations in sediment supply. This study evaluates temporal variations in suspended sedimentdischarge relations for six stations in two selected catchments within the Gamo Highlands in the southern Eth… Show more

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Cited by 8 publications
(7 citation statements)
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“…1/ cos a SCF is the soil crust factor; C is the vegetation cover factor; C (NDVI − NDVI min )/(NDVI max − NDVI min ) Q sf is the amount of wind prevention and sand fixation (t/a); GEP (2023) WF is the climatic erosion factor (kg/m);…”
Section: Wind Prevention and Sand Fixationmentioning
confidence: 99%
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“…1/ cos a SCF is the soil crust factor; C is the vegetation cover factor; C (NDVI − NDVI min )/(NDVI max − NDVI min ) Q sf is the amount of wind prevention and sand fixation (t/a); GEP (2023) WF is the climatic erosion factor (kg/m);…”
Section: Wind Prevention and Sand Fixationmentioning
confidence: 99%
“…The influence degree from different land use types to ESV in Tongling. with the provisions of the Tongling City Urban Master Plan (2016)(2017)(2018)(2019)(2020)(2021)(2022)(2023)(2024)(2025)(2026)(2027)(2028)(2029)(2030) for agricultural and forestry area (1.94 × 10 5 hm 2 ) and built-up land area (4.9 × 10 4 hm 2 ). The finding shows that the selected drivers and the predicted land use layouts are reasonable.…”
Section: Figurementioning
confidence: 99%
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