| Peer-Reviewed

Evaluation of Watershed Characteristics Effects on Stream Flow (A Case of Chacha Watershed, Abay Basin, Ethiopia)

Published in Hydrology (Volume 11, Issue 3)
Received: 31 July 2023    Accepted: 4 October 2023    Published: 14 October 2023
Views:       Downloads:
Abstract

Watershed characteristics of this study includes, land use or land cover, slope, and climate factors are an important factor that affects the streamflow in River basin. The objective of this study was to evaluate the effect of watershed characteristics on stream flow in Chacha watershed of Abay basin. In this study, the streamflow in the Chacha watershed was simulated using the semi-distributed hydrologic model, Soil and Water Assessment Tool (SWAT). The sensitive parameters analysis, SWAT output calibration, and validation for streamflow in the watershed were done using SWAT-CUP (SUFI-2-algorithm). The streamflow was calibrated, and results from calibration show acceptable range (0.88 for R2 and 0.82 for NSE) between observed and simulated stream flow respectively. The results of validation were also acceptable range (0.87 for R2 and 0.81 for NSE). In this study land use and land cover changes, climatic characteristics (rainfall and temperature variation), and slope variation of the topography were having an impact on the streamflow of the Chacha watershed. However, the land use and land cover impact have a more significant influence on the streamflow than other factors. This was due to the stream flow during 2018-LULC was increased by 6.8% over the 1998-LULC. This was the larger percent of increase over the other two factors in the study area. So, to reduce the streamflow in the study area model base land use mitigation measures was done for three basic scenarios by increasing the forest and decreasing the agricultural land with 5%, 10% and 15%. The result shows decreasing annual stream flow by 5.51%, 11.86% and 24.3% for each increment of forest land from the baseline respectively.

Published in Hydrology (Volume 11, Issue 3)
DOI 10.11648/j.hyd.20231103.12
Page(s) 51-61
Creative Commons

This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Streamflow, LULC, Land-Use, Slope, Watershed-Characteristics, Chacha Watershed

References
[1] Alemu, E. (2013). Effects of Watershed characteristics on River Flow for the Case of Ribb And Gummara Catchments. 1–112.
[2] Anctil, F., Lauzon, N., Andréassian, V., Oudin, L., & Perrin, C. (2008). Improvement of rainfall-runoff forecasts through mean areal rainfall optimization. Journal of Hydrology, 328 (3–4), 717–725.
[3] Andréassian, V., Perrin, C., Michel, C., Usart-Sanchez, I., & Lavabre, J. (2001). Impact of imperfect rainfall knowledge on the efficiency and the parameters of watershed models. Journal of Hydrology, 250 (1–4), 206–223.
[4] Andualem G. and Yonas m. (2008). Prediction of Sediment Inflow to [1] Andualem G. and Yonas m., “Prediction of Sediment Inflow to legedadi Reservoir Using SWAT Watershed and CCHE1D Sediment Transport Models,” Nile Basin Water Eng. Sci. Mag., vol. 1, pp. 65–74, 2008. legedadi Reservoir Usi. Nile Basin Water Engineering Scientific Magazine, 1, 65–74.
[5] Andualem, T. G., & Gebremariam, B. (2018a). Evaluation of Land Use Land Cover Change On Stream Flow: A Case Study of Dedessa Sub Basin, Abay Basin, South Western Ethiopia Sediment Yield Modeling of Dedessa Sub Basin, Abay Basin, South-Western Ethiopia View Project Modeling Runoff and Sediment Yield. August.
[6] Andualem, T. G., & Gebremariam, B. (2018b). Evaluation of Land Use Land Cover Change On Stream Flow: A Case Study of Dedessa Sub Basin, Abay Basin, South Western Ethiopia Sediment Yield Modeling of Dedessa Sub Basin, Abay Basin, South-Western Ethiopia View Project Modeling Runoff and Sediment Yield. September 2018.
[7] Arnold, J. G., Moriasi, D. N., Gassman, P. W., Abbaspour, K. C., White, M. J., Srinivasan, R., Santhi, C., Harmel, R. D., Van Griensven, A., Van Liew, M. W., Kannan, N., & Jha, M. K. (2012). SWAT: Model use, calibration, and validation. Transactions of the ASABE, 55 (4), 1491–1508.
[8] Barbalho, et. a. (2014). Average rainfall estimation: methods performance comparison in the Brazilian semi-arid." (2014).
[9] Bekele, D., Alamirew, T., Kebede, A., Zeleke, G., Assefa, M., & Bekele, D. (2021). Modeling the impacts of land use and land cover dynamics on hydrological processes of the Keleta watershed, Ethiopia processes of the Keleta watershed, Ethiopia. Sustainable Environment, 7 (1).
[10] Bewket and Woldeamlak. (2002). Land Cover Dynamics Since the 1950s in Chemoga Watershed, Blue Nile Basin, Ethiopia. 22 (3), 263–269.
[11] Bezawit A. (2011). Discharge and Sediment Yield Modeling in Enkulal Watershed, Lake Tana Region, Ethiopia. 13 (1), 43–50.
[12] Chaubey, I., Cotter, A. S., Costello, T. A., & Soerens, T. S. (2005). Effect of DEM data resolution on SWAT output uncertainty. Hydrological Processes, 19 (3), 621–628.
[13] Chekol, D. A., Tischbein, B., Eggers, H., & Vlek, P. (2007). Application of SWAT for assessment of spatial distribution of water resources and analyzing impact of different land management practices on soil erosion in Upper Awash River Basin watershed. Water Resources, 110–117.
[14] Easton, Z. M., Fuka, D. R., White, E. D., Collick, A. S., Ashagre, B. B., Mccartney, M., & Awulachew, S. B. (2010). Sciences A multi basin SWAT model analysis of runoff and sedimentation in the Blue Nile, Ethiopia. 1827–1841.
[15] Garzanti, E., Andò, S., Vezzoli, G., Ali Abdel Megid, A., & El Kammar, A. (2008). Petrology of Nile River sands (Ethiopia and Sudan): Sediment budgets and erosion patterns. Earth and Planetary Science Letters, 252 (3–4), 327–341.
[16] Geremew, A. A. (2013). Assessing The Impacts of Land Use and Land Cover Change On Hydrology of Watershed: Assessing The Impacts of Land Use and Land Cover Change On Hydrology of Watershed: A Case Study On Gilgel – Abbay Watershed, Lake Tana. 82.
[17] Getachew, H. E., & Melesse, A. M. (2012). The Impact of Land Use Change on the Hydrology of the Angereb Watershed, Ethiopia. January.
[18] Ghonchepour. et. al. (2021). A methodological framework for the hydrological model selection process in water resource management projects. Natural Resource Modeling, 34 (3).
[19] Hassen, E. E., & Assen, M. (2017). Land use / cover dynamics and its drivers in Gelda catchment, Lake Tana watershed,. Environmental Systems Research.
[20] Jain, S., Jain, S., Jain, N., & Xu, C.-Y. (2017). Hydrologic modeling of a Himalayan mountain basin by using the SWAT mode. Hydrology and Earth System Sciences Discussions, March, 1–26.
[21] Khalid, K., Ali, M. F., Rahman, N. F. A., Mispan, M. R., Haron, S. H., Othman, Z., & Bachok, M. F. (2018). Sensitivity Analysis in Watershed Model Using SUFI-2 Algorithm. Procedia Engineering, 162, 441–447.
[22] Mengie, B., Teshome, Y., & Dereje, T. (2019). Effects of soil and water conservation practices on soil physicochemical properties in Gumara watershed, Upper. Ecological Processes, 1–14.
[23] Neitsch, S., Arnold, J.., Kiniry, J.., & Williams, J. (2011). Soil & Water Assessment Tool Theoretical Documentation Version 2009. Texas Water Resources Institute, 1–647.
[24] Rientjes, T. H. M., Haile, A. T., Kebede, E., Mannaerts, C. M. M., Habib, E., & Steenhuis, T. S. (2011). Changes in land cover, rainfall and stream flow in Upper Gilgel Abbay catchment, Blue Nile basin – Ethiopia. 2008, 1979–1989.
[25] Seleshi B. Awlachew, et. a. (2008). Blue Nile flow, Sediment & Impact of Watershed Interventions: Case of Gumera Watershed Seleshi. Biotechnologia Aplicada, 23 (3), 202–210.
[26] Setegn, S. G., Srinivasan, R., & Dargahi, B. (2008). Hydrological Modelling in the Lake Tana Basin, Ethiopia Using SWAT Model. The Open Hydrology Journal, 2 (1), 49–62.
[27] Shawul, A. A., Alamirew, T., & Dinka, M. O. (2013). Calibration and validation of SWAT model and estimation of water balance components of Shaya mountainous watershed, Southeastern Ethiopia. Hydrology and Earth System Sciences Discussions, 10 (11), 13955–13978.
[28] Tadele, K., & Förch, G. (2007). Impact of land use/cover change on streamflow: the case of Hare River Watershed, Ethiopia. Symposium (LARS), Arba Minch, Ethiopia, April 2015, 80–85.
[29] WaleWorqlul, A., Taddele, Y. D., Ayana, E. K., Jeong, J., Adem, A. A., & Gerik, T. (2018). Impact of climate change on streamflow hydrology in headwater catchments of the upper Blue Nile Basin, Ethiopia. Water (Switzerland), 10 (2).
[30] Welde, K., & Gebremariam, B. (2017a). Effect of land use land cover dynamics on hydrological response of watershed: Case study of Tekeze Dam watershed, northern Ethiopia. International Soil and Water Conservation Research, 5 (1), 1–16.
[31] Welde, K., & Gebremariam, B. (2017b). International Soil and Water Conservation Research E ff ect of land use land cover dynamics on hydrological response of watershed : Case study of Tekeze Dam watershed, northern Ethiopia. International Soil and Water Conservation Research, 5 (1), 1–16.
[32] Younger. et al. (2010). Detecting the effects of spatial variability of rainfall on hydrological modelling within an uncertainty analysis framework’, Journal of Hydrology, 2274 (November 2008), pp. 2267–2274.
[33] Sanusi, Wahidah et al. 2017. “Comparison of the Methods to Estimate Missing Values in Monthly Precipitation Data.” International Journal on Advanced Science, Engineering and Information Technology 7 (6): 2168–74.
[34] Lenhart, T. 2015. “Comparison of Two Different Approaches for Making Design Sensitivity Analysis an Integrated Part of Finite Element Analysis.” Structural Optimization 3 (3): 149–56.
[35] Santhi. C. et. al. 2012. “Validation of the SWAT Model on Large River Basin with Point and Nonpoint Sources.” Archives Italiennes de Biologie 112 (1): 18–32.
Cite This Article
  • APA Style

    Getnet Solomon Temtime. (2023). Evaluation of Watershed Characteristics Effects on Stream Flow (A Case of Chacha Watershed, Abay Basin, Ethiopia). Hydrology, 11(3), 51-61. https://doi.org/10.11648/j.hyd.20231103.12

    Copy | Download

    ACS Style

    Getnet Solomon Temtime. Evaluation of Watershed Characteristics Effects on Stream Flow (A Case of Chacha Watershed, Abay Basin, Ethiopia). Hydrology. 2023, 11(3), 51-61. doi: 10.11648/j.hyd.20231103.12

    Copy | Download

    AMA Style

    Getnet Solomon Temtime. Evaluation of Watershed Characteristics Effects on Stream Flow (A Case of Chacha Watershed, Abay Basin, Ethiopia). Hydrology. 2023;11(3):51-61. doi: 10.11648/j.hyd.20231103.12

    Copy | Download

  • @article{10.11648/j.hyd.20231103.12,
      author = {Getnet Solomon Temtime},
      title = {Evaluation of Watershed Characteristics Effects on Stream Flow (A Case of Chacha Watershed, Abay Basin, Ethiopia)},
      journal = {Hydrology},
      volume = {11},
      number = {3},
      pages = {51-61},
      doi = {10.11648/j.hyd.20231103.12},
      url = {https://doi.org/10.11648/j.hyd.20231103.12},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.hyd.20231103.12},
      abstract = {Watershed characteristics of this study includes, land use or land cover, slope, and climate factors are an important factor that affects the streamflow in River basin. The objective of this study was to evaluate the effect of watershed characteristics on stream flow in Chacha watershed of Abay basin. In this study, the streamflow in the Chacha watershed was simulated using the semi-distributed hydrologic model, Soil and Water Assessment Tool (SWAT). The sensitive parameters analysis, SWAT output calibration, and validation for streamflow in the watershed were done using SWAT-CUP (SUFI-2-algorithm). The streamflow was calibrated, and results from calibration show acceptable range (0.88 for R2 and 0.82 for NSE) between observed and simulated stream flow respectively. The results of validation were also acceptable range (0.87 for R2 and 0.81 for NSE). In this study land use and land cover changes, climatic characteristics (rainfall and temperature variation), and slope variation of the topography were having an impact on the streamflow of the Chacha watershed. However, the land use and land cover impact have a more significant influence on the streamflow than other factors. This was due to the stream flow during 2018-LULC was increased by 6.8% over the 1998-LULC. This was the larger percent of increase over the other two factors in the study area. So, to reduce the streamflow in the study area model base land use mitigation measures was done for three basic scenarios by increasing the forest and decreasing the agricultural land with 5%, 10% and 15%. The result shows decreasing annual stream flow by 5.51%, 11.86% and 24.3% for each increment of forest land from the baseline respectively.},
     year = {2023}
    }
    

    Copy | Download

  • TY  - JOUR
    T1  - Evaluation of Watershed Characteristics Effects on Stream Flow (A Case of Chacha Watershed, Abay Basin, Ethiopia)
    AU  - Getnet Solomon Temtime
    Y1  - 2023/10/14
    PY  - 2023
    N1  - https://doi.org/10.11648/j.hyd.20231103.12
    DO  - 10.11648/j.hyd.20231103.12
    T2  - Hydrology
    JF  - Hydrology
    JO  - Hydrology
    SP  - 51
    EP  - 61
    PB  - Science Publishing Group
    SN  - 2330-7617
    UR  - https://doi.org/10.11648/j.hyd.20231103.12
    AB  - Watershed characteristics of this study includes, land use or land cover, slope, and climate factors are an important factor that affects the streamflow in River basin. The objective of this study was to evaluate the effect of watershed characteristics on stream flow in Chacha watershed of Abay basin. In this study, the streamflow in the Chacha watershed was simulated using the semi-distributed hydrologic model, Soil and Water Assessment Tool (SWAT). The sensitive parameters analysis, SWAT output calibration, and validation for streamflow in the watershed were done using SWAT-CUP (SUFI-2-algorithm). The streamflow was calibrated, and results from calibration show acceptable range (0.88 for R2 and 0.82 for NSE) between observed and simulated stream flow respectively. The results of validation were also acceptable range (0.87 for R2 and 0.81 for NSE). In this study land use and land cover changes, climatic characteristics (rainfall and temperature variation), and slope variation of the topography were having an impact on the streamflow of the Chacha watershed. However, the land use and land cover impact have a more significant influence on the streamflow than other factors. This was due to the stream flow during 2018-LULC was increased by 6.8% over the 1998-LULC. This was the larger percent of increase over the other two factors in the study area. So, to reduce the streamflow in the study area model base land use mitigation measures was done for three basic scenarios by increasing the forest and decreasing the agricultural land with 5%, 10% and 15%. The result shows decreasing annual stream flow by 5.51%, 11.86% and 24.3% for each increment of forest land from the baseline respectively.
    VL  - 11
    IS  - 3
    ER  - 

    Copy | Download

Author Information
  • Department of Hydraulic and Water Resource Engineering, Kombolcha Institute of Technology Wollo University, Kombolcha, Ethiopia

  • Sections