ANALYSIS AND CHARACTERIZATION OF HYDROLOGICAL DROUGHT UNDER CLIMATE CHANGE IN HAMASSA WATERSHED, RIFT VALLEY BASIN
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Date
2024-07-20
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Hawassa University
Abstract
Hydrological drought occurs when there is an extended period of significantly reduced water
availability, leading to depleted water sources and severe impacts on ecosystem and
communities. Water scarcity caused by prolonged periods of reduced rainfall due to climate
change can lead to the natural disaster of drought. However, little has been done so far on
hydrological drought under climate change in Hamassa watershed. This study aimed to
analyze and characterize hydrological drought under climate change in the Hamassa
watershed, Rift Valley Basin, Ethiopia. Hydrological data (1992-2015), meteorological data
(1992-2022), future climate data 2030-2090), spatial data, DEM, land use land cover, and
soil were collected. CMhyd software package was used for bias correction of the climate
data. The hydrological model soil and water assessment tool (SWAT) was used for
hydrological analysis. The simulation result was calibrated and validated using the SWAT
calibration uncertainty procedure (SWAT-CUP). Standard precipitation index (SPI) and
stream flow drought index (SDI) are used to decide drought conditions in a watershed and
to identify drought-prone areas in the watershed. Temperature projections for both the near
and long term indicate an increase compared to the current period under both RCP2.6 and
RCP8.5 scenarios. Meanwhile, precipitation projections suggest a decrease for the periods
2040-2060 and 2061-2072 under both RCP2.6 and RCP8.5 scenarios. The standard
precipitation index (SPI) and stream flow drought index (SDI) results showed that the
watershed experiences mild (-0.5- -0.999), moderate (-1- -1.49), severe (-1.5- -1.99), and
extreme (≤ - 2) drought events. Droughts are projected to occur in the periods 2040-2060
and 2061-2072 under both RCP2.6 and RCP8.5 scenarios. Sub-watersheds 7, 8, 9, 10, and
11 showed high vulnerability to severe and extreme drought. Drought-mitigating structures
are needed to mitigate drought in the watershed
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Keywords
Climate Change, CMhyd, SDI, SPI, SWAT model, SWAT-CUP
