Spatial distribution and temporal trends of rainfall and erosivity in the Eastern Africa region

  • Ayele Almaw Fenta
    Arid Land Research Center Tottori University 1390 Hamasaka Tottori 680–0001 Japan
  • Hiroshi Yasuda
    Arid Land Research Center Tottori University 1390 Hamasaka Tottori 680–0001 Japan
  • Katsuyuki Shimizu
    Faculty of Agriculture Tottori University 4–101 Koyama‐cho Minami Tottori 680–8553 Japan
  • Nigussie Haregeweyn
    International Platform for Dryland Research and Education Tottori University 1390 Hamasaka Tottori 680–0001 Japan
  • Takayuki Kawai
    Arid Land Research Center Tottori University 1390 Hamasaka Tottori 680–0001 Japan
  • Dagnenet Sultan
    Arid Land Research Center Tottori University 1390 Hamasaka Tottori 680–0001 Japan
  • Kindiye Ebabu
    Arid Land Research Center Tottori University 1390 Hamasaka Tottori 680–0001 Japan
  • Ashebir Sewale Belay
    Department of Earth Science Bahir Dar University P.O. Box 79 Bahir Dar Ethiopia

説明

<jats:title>Abstract</jats:title><jats:p>Soil erosion by water is one of the main environmental concerns in the drought‐prone Eastern Africa region. Understanding factors such as rainfall and erosivity is therefore of utmost importance for soil erosion risk assessment and soil and water conservation planning. In this study, we evaluated the spatial distribution and temporal trends of rainfall and erosivity for the Eastern Africa region during the period 1981–2016. The precipitation concentration index, seasonality index, and modified Fournier index have been analysed using 5 × 5‐km resolution multisource rainfall product (Climate Hazards Group InfraRed Precipitation with Stations). The mean annual rainfall of the region was 810 mm ranging from less than 300 mm in the lowland areas to over 1,200 mm in the highlands being influenced by orography of the Eastern Africa region. The precipitation concentration index and seasonality index revealed a spatial pattern of rainfall seasonality dependent on latitude, with a more pronounced seasonality as we go far from the equator. The modified Fournier index showed high spatial variability with about 55% of the region subject to high to very high rainfall erosivity. The mean annual R‐factor in the study region was calculated at 3,246 ± 1,895 MJ mm ha<jats:sup>−1</jats:sup> h<jats:sup>−1</jats:sup> yr<jats:sup>−1</jats:sup>, implying a potentially high water erosion risk in the region. Moreover, both increasing and decreasing trends of annual rainfall and erosivity were observed but spatial variability of these trends was high. This study offers useful information for better soil erosion prediction as well as can support policy development to achieve sustainable regional environmental planning and management of soil and water resources.</jats:p>

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