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Climate Profile Over Jeldu Woreda of West Shewa Zone, Oromia, Ethiopia

Received: 2 August 2024     Accepted: 27 August 2024     Published: 23 September 2024
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Abstract

Identifying the climate profile of an area is essential for effective water resource management, agricultural planning and disaster preparedness. This study focuses on characterizing rainfall patterns and identifying the variability of Jeldu woreda in Oromia, Ethiopia. Previously and recently, little study tried to show the woreda profile, which did not bases on station data properly. Forty years (1981-2020) of stations’ rainfall and temperature data were utilized. The study area had natural forest, highland and mid land with varying topography. Based on the annual rainfall cycle, the woreda had bi-modal rainfall types, with the peak of the year being July. Statistical methods and python script were applied to identify the climate profile. The results show that main rainy seasonal rainfall starts on average from 12-14 June and ceases averagely around 10-15 October. During second rainy period, the rain starts from 25 February to 10 March. The mean annual rainfall of woreda is 1395.1 mm, and the average maximum temperature is 19.5°. Kiremt contributes the highest percent, which is more than 64 % of the annual total rainfall. The 1987 and 2015 were the driest years, and 1996 and 2010 is the wettest during kiremt, 1987 and 2010 the wettest, and 1999 and 2015 the driest during Belg. Seasonal rainfall had a regular to moderate precipitation concentration over woreda. Identifying the causes of unseasonal rainfall that happened during dry season over the study area can help to decrease weather hazard during the season.

Published in Science Discovery (Volume 12, Issue 5)
DOI 10.11648/j.sd.20241205.12
Page(s) 114-121
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

Woreda, Climate Profile, Characterizing, Rainy Season

References
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[2] S. S. Tesfaye, “Analysis of farmers perception on the impact of land degradation hazard on agricultural land productivity in Jeldu district in West Shewa Zone, Oromia, Ethiopia,” J. Agric. Ext. Rural Dev., vol. 9, no. 6, pp. 111–123, 2017,
[3] Z. T. Segele and P. J. Lamb, “Characterization and variability of Kiremt rainy season over Ethiopia,” Meteorol. Atmos. Phys., vol. 89, no. 1–4, pp. 153–180, 2005,
[4] T. Dinku et al., “Enhancing National Climate Services (ENACTS) for development in Africa,” Clim. Dev., pp. 1–9, Nov. 2017,
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[6] K. T. Zeleke, “Analysis of rainfall climate and evapo-transpiration in arid and semi-arid regions of Ethiopia using data over the last half a century Analysis of rainfall climate and evapo-transpiration in arid and semi-arid regions of Ethiopia using data over the last,” no. November, 2019,
[7] A. T. Game and D. Korecha, “Recent Changes in Rainfall, Temperature and Number of Rainy Days over Northern Oromia Zone , Ethiopia,” vol. 3, no. 6, pp. 62–70, 2015,
[8] Z. T. Segele, P. J. Lamb, and L. M. Leslie, “Ensemble-Based Statistical Prediction of Ethiopian Monthly-to- Seasonal Kiremt Rainfall”.
[9] A. Asfaw, B. Simane, A. Hassen, and A. Bantider, “Variability and time series trend analysis of rainfall and temperature in northcentral Ethiopia: A case study in Woleka sub-basin,” Weather Clim. Extrem., vol. 19, no. December 2017, pp. 29–41, 2018,
[10] M. De Luis, J. C. González-Hidalgo, M. Brunetti, and L. A. Longares, “Precipitation concentration changes in Spain 1946-2005,” Nat. Hazards Earth Syst. Sci., vol. 11, no. 5, pp. 1259–1265, 2011,
[11] K. Koudahe, A. J. Kayode, A. O. Samson, A. A. Adebola, and K. Djaman, “Trend Analysis in Standardized Precipitation Index and Standardized Anomaly Index in the Context of Climate Change in Southern Togo,” Atmos. Clim. Sci., vol. 07, no. 04, pp. 401–423, 2017,
[12] S. Brahimi, H. Meddi, M. Meddi, F. Hallouz, and A. Saaed Hamoudi, “The Precipitation Concentration in the Cheliff Watershed, Algeria: A Critical Analysis for Sustainable Water Resource Management,” Chinese J. Urban Environ. Stud., vol. 11, no. 3, 2023,
[13] K. Zhang, Y. Yao, X. Qian, and J. Wang, “Various characteristics of precipitation concentration index and its cause analysis in China between 1960 and 2016,” Int. J. Climatol., vol. 39, no. 12, pp. 4648–4658, 2019,
[14] D. Bekele, T. Alamirew, A. Kebede, G. Zeleke, and A. M. Melese, “Analysis of rainfall trend and variability for agricultural water management in Awash River Basin, Ethiopia,” J. Water Clim. Chang., vol. 8, no. 1, pp. 127–141, 2017.
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  • APA Style

    Wami, A. H., Balcha, G. D., Game, A. T. (2024). Climate Profile Over Jeldu Woreda of West Shewa Zone, Oromia, Ethiopia. Science Discovery, 12(5), 114-121. https://doi.org/10.11648/j.sd.20241205.12

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    ACS Style

    Wami, A. H.; Balcha, G. D.; Game, A. T. Climate Profile Over Jeldu Woreda of West Shewa Zone, Oromia, Ethiopia. Sci. Discov. 2024, 12(5), 114-121. doi: 10.11648/j.sd.20241205.12

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    AMA Style

    Wami AH, Balcha GD, Game AT. Climate Profile Over Jeldu Woreda of West Shewa Zone, Oromia, Ethiopia. Sci Discov. 2024;12(5):114-121. doi: 10.11648/j.sd.20241205.12

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  • @article{10.11648/j.sd.20241205.12,
      author = {Abdisa Hirko Wami and Gashawun Dereje Balcha and Asaminew Tashome Game},
      title = {Climate Profile Over Jeldu Woreda of West Shewa Zone, Oromia, Ethiopia
    },
      journal = {Science Discovery},
      volume = {12},
      number = {5},
      pages = {114-121},
      doi = {10.11648/j.sd.20241205.12},
      url = {https://doi.org/10.11648/j.sd.20241205.12},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.sd.20241205.12},
      abstract = {Identifying the climate profile of an area is essential for effective water resource management, agricultural planning and disaster preparedness. This study focuses on characterizing rainfall patterns and identifying the variability of Jeldu woreda in Oromia, Ethiopia. Previously and recently, little study tried to show the woreda profile, which did not bases on station data properly. Forty years (1981-2020) of stations’ rainfall and temperature data were utilized. The study area had natural forest, highland and mid land with varying topography. Based on the annual rainfall cycle, the woreda had bi-modal rainfall types, with the peak of the year being July. Statistical methods and python script were applied to identify the climate profile. The results show that main rainy seasonal rainfall starts on average from 12-14 June and ceases averagely around 10-15 October. During second rainy period, the rain starts from 25 February to 10 March. The mean annual rainfall of woreda is 1395.1 mm, and the average maximum temperature is 19.5°. Kiremt contributes the highest percent, which is more than 64 % of the annual total rainfall. The 1987 and 2015 were the driest years, and 1996 and 2010 is the wettest during kiremt, 1987 and 2010 the wettest, and 1999 and 2015 the driest during Belg. Seasonal rainfall had a regular to moderate precipitation concentration over woreda. Identifying the causes of unseasonal rainfall that happened during dry season over the study area can help to decrease weather hazard during the season.
    },
     year = {2024}
    }
    

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  • TY  - JOUR
    T1  - Climate Profile Over Jeldu Woreda of West Shewa Zone, Oromia, Ethiopia
    
    AU  - Abdisa Hirko Wami
    AU  - Gashawun Dereje Balcha
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    DO  - 10.11648/j.sd.20241205.12
    T2  - Science Discovery
    JF  - Science Discovery
    JO  - Science Discovery
    SP  - 114
    EP  - 121
    PB  - Science Publishing Group
    SN  - 2331-0650
    UR  - https://doi.org/10.11648/j.sd.20241205.12
    AB  - Identifying the climate profile of an area is essential for effective water resource management, agricultural planning and disaster preparedness. This study focuses on characterizing rainfall patterns and identifying the variability of Jeldu woreda in Oromia, Ethiopia. Previously and recently, little study tried to show the woreda profile, which did not bases on station data properly. Forty years (1981-2020) of stations’ rainfall and temperature data were utilized. The study area had natural forest, highland and mid land with varying topography. Based on the annual rainfall cycle, the woreda had bi-modal rainfall types, with the peak of the year being July. Statistical methods and python script were applied to identify the climate profile. The results show that main rainy seasonal rainfall starts on average from 12-14 June and ceases averagely around 10-15 October. During second rainy period, the rain starts from 25 February to 10 March. The mean annual rainfall of woreda is 1395.1 mm, and the average maximum temperature is 19.5°. Kiremt contributes the highest percent, which is more than 64 % of the annual total rainfall. The 1987 and 2015 were the driest years, and 1996 and 2010 is the wettest during kiremt, 1987 and 2010 the wettest, and 1999 and 2015 the driest during Belg. Seasonal rainfall had a regular to moderate precipitation concentration over woreda. Identifying the causes of unseasonal rainfall that happened during dry season over the study area can help to decrease weather hazard during the season.
    
    VL  - 12
    IS  - 5
    ER  - 

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