Version 1
: Received: 20 July 2023 / Approved: 21 July 2023 / Online: 24 July 2023 (10:57:56 CEST)
How to cite:
Chala, H.M.; Tegene, W.D.; Niguse, A.G. CLIMATE CHANGE IMPACT ON THE WATER RESOURCE OF ARBA RIVER CATCHMENT, AWASH RIVER BASIN, ETHIOPIA. Preprints2023, 2023071549. https://doi.org/10.20944/preprints202307.1549.v1
Chala, H.M.; Tegene, W.D.; Niguse, A.G. CLIMATE CHANGE IMPACT ON THE WATER RESOURCE OF ARBA RIVER CATCHMENT, AWASH RIVER BASIN, ETHIOPIA. Preprints 2023, 2023071549. https://doi.org/10.20944/preprints202307.1549.v1
Chala, H.M.; Tegene, W.D.; Niguse, A.G. CLIMATE CHANGE IMPACT ON THE WATER RESOURCE OF ARBA RIVER CATCHMENT, AWASH RIVER BASIN, ETHIOPIA. Preprints2023, 2023071549. https://doi.org/10.20944/preprints202307.1549.v1
APA Style
Chala, H.M., Tegene, W.D., & Niguse, A.G. (2023). CLIMATE CHANGE IMPACT ON THE WATER RESOURCE OF ARBA RIVER CATCHMENT, AWASH RIVER BASIN, ETHIOPIA. Preprints. https://doi.org/10.20944/preprints202307.1549.v1
Chicago/Turabian Style
Chala, H.M., Wegayehu Demise Tegene and Abera Girma Niguse. 2023 "CLIMATE CHANGE IMPACT ON THE WATER RESOURCE OF ARBA RIVER CATCHMENT, AWASH RIVER BASIN, ETHIOPIA" Preprints. https://doi.org/10.20944/preprints202307.1549.v1
Abstract
This study was investigate the possible hydrological impact of climate change in stream flow of Arba River based on the downscaled precipitation and temperature data at West Harerghe Zone, Oromia regional state, Ethiopia. The case study, Arba River is one of the tributaries of Awash River Basin and the catchment of the river at Bordode flow gauging station covers around 72 square kilometers. Dynamically downscaled Regional Climate Model (RCM) HIRHAM derived by ICHEC-EC-EARTH global climate model under two scenarios RCP 4.5 and 8.5 was used in this study. The future time periods are divided into two time horizons with equal length of time as the base line period 2021–2050 and 2051–2080. For both projected periods relatively the minimum average monthly percentage change in precipitation will be happened from May to October under RCP4.5 except August and from March to October under RCP8.5. The variation under RCP4.5 is relatively high when compared to RCP8.5. The average monthly per-centage of flow increment may vary from (7.6 to 81.8) for 2021-2050 and (22.3 to 107.8) for 2051-2080 under RCP4.5. Under RCP8.5 scenario, from July to January except the December for 2021-2050, simulated flow is expected to increase while from February to June decreases for both time horizons. Generally, the change of simulated flow under both scenarios and both near and far time period is follows the pattern of precipitation. However, the flow change will have less variation than the precipitation change.
Keywords
climate change; water potential; RCM; Arba River; Ethiopia
Subject
Environmental and Earth Sciences, Water Science and Technology
Copyright:
This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
