Streamflow and Sediment Yield Prediction for Watershed Prioritization in the Upper Blue Nile River Basin, Ethiopia

被引:117
|
作者
Ayele, Gebiaw T. [1 ,2 ]
Teshale, Engidasew Z. [3 ]
Yu, Bofu [1 ,2 ]
Rutherfurd, Ian D. [4 ]
Jeong, Jaehak [5 ]
机构
[1] Griffith Univ, Australian Rivers Inst, Nathan, Qld 4111, Australia
[2] Griffith Univ, Sch Engn, Nathan, Qld 4111, Australia
[3] Ethiopian Minist Water Resources, Addis Ababa 1000, Ethiopia
[4] Univ Melbourne, Sch Geog, Parkville, Vic 3010, Australia
[5] Texas A&M AgriLife Res, Blackland Res & Extens Ctr, 720 East Blackland Rd, Temple, TX 76502 USA
来源
WATER | 2017年 / 9卷 / 10期
关键词
land use change; watershed prioritization; reservoir sedimentation; Blue Nile river basin; sediment yield; SWAT-CUP; AUTOMATIC CALIBRATION; SENSITIVITY-ANALYSIS; SWAT MODEL; UNCERTAINTY; RUNOFF; SOIL; HYDROLOGY; QUALITY; PARAMETERS; TRANSPORT;
D O I
10.3390/w9100782
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Inappropriate use of land and poor ecosystem management have accelerated land degradation and reduced the storage capacity of reservoirs. To mitigate the effect of the increased sediment yield, it is important to identify erosion-prone areas in a 287 km(2) catchment in Ethiopia. The objectives of this study were to: (1) assess the spatial variability of sediment yield; (2) quantify the amount of sediment delivered into the reservoir; and (3) prioritize sub-catchments for watershed management using the Soil and Water Assessment Tool (SWAT). The SWAT model was calibrated and validated using SUFI-2, GLUE, ParaSol, and PSO SWAT-CUP optimization algorithms. For most of the SWAT-CUP simulations, the observed and simulated river discharge were not significantly different at the 95% level of confidence (95PPU), and sources of uncertainties were captured by bracketing more than 70% of the observed data. This catchment prioritization study indicated that more than 85% of the sediment was sourced from lowland areas (slope range: 0-8%) and the variation in sediment yield was more sensitive to the land use and soil type prevailing in the area regardless of the terrain slope. Contrary to the perception of the upland as an important source of sediment, the lowland in fact was the most important source of sediment and should be the focus area for improved land management practice to reduce sediment delivery into storage reservoirs. The research also showed that lowland erosion-prone areas are typified by extensive agriculture, which causes significant modification of the landscape. Tillage practice changes the infiltration and runoff characteristics of the land surface and interaction of shallow groundwater table and saturation excess runoff, which in turn affects the delivery of water and sediment to the reservoir and catchment evapotranspiration.
引用
收藏
页数:29
相关论文
共 50 条
  • [1] Watershed-based soil erosion and sediment yield modeling in the Rib watershed of the Upper Blue Nile Basin, Ethiopia
    Sinshaw, Berhanu G.
    Belete, Abreham M.
    Mekonen, Belachew M.
    Wubetu, Tesgaye G.
    Anley, Tegenu L.
    Alamneh, Wolelaw D.
    Atinkut, Haimanot B.
    Gelaye, Abay A.
    Bilkew, Tenaw
    Tefera, Agumase K.
    Dessie, Abebe Birara
    Fenta, Habtamu M.
    Beyene, Agumas M.
    Bizuneh, Belay B.
    Alem, Habtamu T.
    Eshete, Daniel G.
    Atanaw, Simir B.
    Tebkew, Mekuanent A.
    Birhanu, Mengistie Mossie
    [J]. ENERGY NEXUS, 2021, 3
  • [2] Morphometric analysis: sub-watershed prioritization in the temcha watershed, upper Blue Nile Basin, Ethiopia
    Adam, Tamir
    Fetene, Aramde
    Girma, Million
    [J]. SUSTAINABLE WATER RESOURCES MANAGEMENT, 2024, 10 (04)
  • [3] Streamflow and sediment yield estimation, and area prioritization for better conservation planning in the Dawe River watershed of the Wabi Shebelle River Basin, Ethiopia
    Roba, Negash Tessema
    Kassa, Asfaw Kebede
    Geleta, Dame Yadeta
    Harka, Arus Edo
    [J]. HELIYON, 2021, 7 (12)
  • [4] Climate change and its impact on streamflow in the upper Blue Nile River Basin, Ethiopia
    Kassa, Gizachew
    Dessalegn, Ayenew
    Bhowmick, Anirudh
    [J]. INTERNATIONAL JOURNAL OF HYDROLOGY SCIENCE AND TECHNOLOGY, 2024, 17 (03) : 278 - 297
  • [5] Watershed Hydrological Responses to Land Cover Changes at Muger Watershed, Upper Blue Nile River Basin, Ethiopia
    Teshome, Dawit Samuel
    Leta, Megersa Kebede
    Taddese, Habitamu
    Moshe, Alene
    Tolessa, Terefe
    Ayele, Gebiaw T.
    You, Songcai
    [J]. WATER, 2023, 15 (14)
  • [6] Sediment yield estimation and evaluating the best management practices in Nashe watershed, Blue Nile Basin, Ethiopia
    Leta, Megersa Kebede
    Waseem, Muhammad
    Rehman, Khawar
    Traenckner, Jens
    [J]. ENVIRONMENTAL MONITORING AND ASSESSMENT, 2023, 195 (06)
  • [7] Sediment yield estimation and evaluating the best management practices in Nashe watershed, Blue Nile Basin, Ethiopia
    Megersa Kebede Leta
    Muhammad Waseem
    Khawar Rehman
    Jens Tränckner
    [J]. Environmental Monitoring and Assessment, 2023, 195
  • [8] Watershed-based soil erosion and sediment yield modeling in the Rib watershed of the Upper Blue Nile Basin, Ethiopia (vol 3, 100023, 2021)
    Sinshaw, Berhanu G.
    Belete, Abreham M.
    Mekonen, Belachew M.
    Wubetu, Tesgaye G.
    Anley, Tegenu L.
    Alamneh, Wolelaw D.
    Atinkut, Haimanot B.
    Gelaye, Abay A.
    Bilkew, Tenaw
    Tefera, Agumase K.
    Dessie, Abebe Birara
    Fenta, Habtamu M.
    Beyene, Agumas M.
    Bizuneh, Belay B.
    Alem, Habtamu T.
    Eshete, Daniel G.
    Atanaw, Simir B.
    Tebkew, Mekuanent
    Birhanu, Mengistie Mossie
    [J]. ENERGY NEXUS, 2022, 5
  • [9] Prioritization of watershed management scenarios under climate change in the Jemma sub-basin of the Upper Blue Nile Basin, Ethiopia
    Worku, Gebrekidan
    Teferi, Ermias
    Bantider, Amare
    Dile, Yihun T.
    [J]. JOURNAL OF HYDROLOGY-REGIONAL STUDIES, 2020, 31
  • [10] Sediment yield modeling in Awash Melkasa dam watershed, upper Awash River basin, Ethiopia
    Daba, Bayisa Itana
    Demissie, Tamene Adugna
    Tufa, Fayera Gudu
    [J]. ACTA GEOPHYSICA, 2023, 71 (05) : 2287 - 2306