Evaluation of the Impacts of Climate Change on Sediment Yield from the Logiya Watershed, Lower Awash Basin, Ethiopia

Nura Boru Jilo,Fiseha Behulu,Arus Edo Harka,Bogale Gebremariam,Gezahegn Weldu Woldemariam

doi:10.3390/hydrology6030081

Abstract

It is anticipated that climate change will impact sediment yield in watersheds. The purpose of this study was to investigate the impacts of climate change on sediment yield from the Logiya watershed in the lower Awash Basin, Ethiopia. Here, we used the coordinated regional climate downscaling experiment (CORDEX)-Africa data outputs of Hadley Global Environment Model 2-Earth System (HadGEM2-ES) under representative concentration pathway (RCP) scenarios (RCP4.5 and RCP8.5). Future scenarios of climate change were analyzed in two-time frames: 2020–2049 (2030s) and 2050–2079 (2060s). Both time frames were analyzed using both RCP scenarios from the baseline period (1971–2000). A Soil and Water Assessment Tool (SWAT) model was constructed to simulate the hydrological and the sedimentological responses to climate change. The model performance was calibrated and validated using the coefficient of determination (R2), Nash–Sutcliffe efficiency (NSE), and percent bias (PBIAS). The results of the calibration and the validation of the sediment yield R2, NSE, and PBIAS were 0.83, 0.79, and −23.4 and 0.85, 0.76, and −25.0, respectively. The results of downscaled precipitation, temperature, and estimated evapotranspiration increased in both emission scenarios. These climate variable increments were expected to result in intensifications in the mean annual sediment yield of 4.42% and 8.08% for RCP4.5 and 7.19% and 10.79% for RCP8.5 by the 2030s and the 2060s, respectively.

Highlights

Climate change is becoming a major environmental concern because increasing scientific evidence shows the high concentration of greenhouse gases (GHGs) in the atmosphere, and frequent hydro-meteorological extreme events are becoming the 21st century phenomenon [1,2]
Results indicated thatRCP4.5 for RCP4.5 and RCP8.5, the maximum minimum sediment loads loads of the watershed occurredoccurred in the sub-watersheds
For the RCP8.5 scenario, the model showed an increase of 2.81% by the 2030s and

Summary

Introduction

Climate change is becoming a major environmental concern because increasing scientific evidence shows the high concentration of greenhouse gases (GHGs) in the atmosphere, and frequent hydro-meteorological extreme events are becoming the 21st century phenomenon [1,2]. The consequences of climate change involve adverse impacts on environment, hydrological cycle, water resources, agriculture and food security, human health, terrestrial ecosystems, and biodiversity [3,4,5,6,7,8]. These events are mostly manifested through subsequent influences of climate variables, including precipitation, temperature, and evapotranspiration [9,10,11].

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Discussion

Conclusion