Abstract

Soil erosion represents one of the most important global issues with serious effects on agriculture and water quality, especially in developing countries, such as Ethiopia, where rapid population growth and climatic changes affect widely mountainous areas. The Meskay catchment is a head catchment of the Jemma Basin draining into the Blue Nile (Central Ethiopia) and is characterized by high relief energy. Thus, it is exposed to high degradation dynamics, especially in the lower parts of the catchment. In this study, we aim at the geomorphological assessment of soil erosion susceptibilities. First, a geomorphological map was generated based on remote sensing observations. In particular, we mapped three categories of landforms related to (i) sheet erosion, (ii) gully erosion, and (iii) badlands using a high-resolution digital elevation model (DEM). The map was validated by a detailed field survey. Subsequently, we used the three categories as dependent variables in a probabilistic modelling approach to derive the spatial distribution of the specific process susceptibilities. In this study we applied the maximum entropy model (MaxEnt). The independent variables were derived from a set of spatial attributes describing the lithology, terrain, and land cover based on remote sensing data and DEMs. As a result, we produced three separate susceptibility maps for sheet and gully erosion as well as badlands. The resulting susceptibility maps showed good to excellent prediction performance. Moreover, to explore the mutual overlap of the three susceptibility maps, we generated a combined map as a color composite where each color represents one component of water erosion. The latter map yields useful information for land-use managers and planning purposes.

Highlights

  • Erosion is a natural process levelling the relief of the landscape

  • The results show that ELEV highly influences the three models presenting a percent contribution (PC) > 20%

  • The present study demonstrates that maximum entropy (MaxEnt) is suitable for the evaluation of water erosion susceptibility and produced models with satisfying accuracy and predictive performances

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Summary

Introduction

Erosion is a natural process levelling the relief of the landscape. Its intensity is influenced by weather extremes and environmental conditions. In areas exposed to weather extremes, such as heavy rainfall events followed by dry periods, sheet and gully erosion, as well as Badland formation, could appear. These forms develop due to a complex interplay of driving forces, such as tectonics, the nature of soils, slope characteristics, land cover, and land use, as well as the aforementioned climatic conditions [1]. The actual landscape shows deeply incised gorges characterized by over-steepened unstable slopes [4,5]

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