Land Degradation Dynamics Under Land Use Land Cover and Climate Change Projection Towards the Appraisal of Potential Soil and Water Conservation Practices in the Gidabo Watershed, Ethiopian Rift Valley Lakes Basin
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Date
2024-10-11
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Hawassa University
Abstract
The intricate relationship between land use, climate dynamics, and land degradation profoundly
impacts the sustainability of ecosystems and human well-being in Ethiopia. This study,
conducted in the Gidabo Watershed (GW) within the Ethiopian Rift Valley Lakes Basin
(ERVLB), aimed to assess the long-term land use land cover (LULC), evaluate regional climate
models (RCMs), assess land degradation indicators, and propose management alternatives. To
address these objectives, multidisciplinary approach integrating, remote sensing, geospatial
analysis, statistical metrics and hydrological modeling were used. The study identified nine
major LULC classes i.e., water body, grass land, forest, agriculture, bare/barren land, built-up,
agroforestry, shrub and marsh land. The watershed experienced significant LULC changes
between 1985 and 2021, predominantly driven by agricultural expansion at the expense of
forest, shrub, and grasslands. Future (2035 and 2050) projections using a hybrid Multi-Layer
Perceptron (MLP) and Cellular Automata-Markov chain (CA-MC) model indicated further
agricultural expansion, accompanied by declines in forest and grasslands. Furthermore, the
study evaluated 11 CORDEX-Africa RCMs and their mean ensemble performance, revealing
varied accuracies in reproducing rainfall and temperature patterns over GW from 1991 to 2005.
The observed climate trends indicated a significant declining rainfall (-13.38 mm/year) and
warming temperatures, with future projections (RCP4.5 and RCP8.5) showing consistent
temperature increases. Additionally, the study investigated the impact of LULC and climate
change on surface runoff and sediment yield using SWAT model. The results revealed notable
increases in surface runoff and sediment yield attributed to LULC changes. Whereas, climate
change alone exhibited a diverse influence, with both increases and decreases in surface runoff
and sediment yield. Similarly, the combined effects of LULC and climate change demonstrated
that certain scenarios led to the increases in surface runoff and sediment yield, while others
reduced these processes. This might be attributed to the offset of runoff and sediment reduction
by climate change. Soil erosion rates were found to be high, particularly most of the southern
and eastern parts of the watershed will generate the highest amount of surface runoff and
sediment yield in to the future. Addressing these concerns, soil/stone bund, terracing, contour
farming, and reforestation practice can significantly reduce the annual sediment yield in the
future. The land degradation neutrality (LDN) assessment from 1985–2003 to 2003–2021
revealed land productivity decline, land cover degradation, SOC loss, and the expansion of land
degradation trajectories by 26%. Overall, the findings provide valuable information for stakeholders.
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Keywords
climate change, land use, soil erosion, land degradation, soil conservation practice
