Multi-model ensemble of CMIP6 projections for past and future climate change on mean precipitation and temperature

High-resolution climatic Projections are increasingly essential for informed decision-making and efficient adaptation and mitigation planning, especially in climatically sensitive regions such as the Baro River sub-basin in Ethiopia. This study applied station observation data with systematic bias correction utilizing quantile mapping. Historical and future climate trends were analyzed using multi-model ensembles from high-resolution Coupled Model Intercomparison Project phase 6 (CMIP6) under two Shared Socioeconomic Pathways (SSP2-4.5 and SSP5-8.5). The non-parametric Mann–Kendall test and Sen’s Slope estimator were used to detect trends in the 21st century. Historical records (1986–2014) reveal a distinct seasonal rainfall pattern, with peak rainfall occurring in July and August. Projections for the late 21st century (2081–2100) suggest significant increases in mean monthly rainfall by 20.6% (159.1 mm/month) under SSP2-4.5 and by 46.7% (193.5 mm/month) under SSP5-8.5 compared to the historical baseline (132.0 mm/month). Station-level analysis reveals pronounced spatial variability, with substantial increases in rainfall at Lare (+ 129.99%) and Gambella (+ 103.09%) under SSP5-8.5, while other stations show slight increases or even negative trends. Mean annual temperatures are projected to rise by up to 7.16% (reaching 23.69 °C) under SSP2-4.5 and by 18.83% (up to 26.27 °C) under SSP5-8.5, with anomalies reaching as high as 6 °C by the end of the century. Probability density function analysis indicates a shift toward greater variability and more extreme events, mostly under SSP5-8.5. Rainfall distributions exhibit increasing bimodality, while temperature distributions demonstrate widening, indicating a higher likelihood of extreme drought and extreme hot and wet years. These findings emphasize how vulnerable the Baro River Sub-Basin is to hydro-climatic extremes and highlight the urgent need for emissions mitigation and developing strong, tailored adaptation strategies for the area.

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Journal
ENVIRONMENTAL SYSTEMS RESEARCH
Published
2025-12-01
DOI
https://doi.org/10.1186/s40068-025-00422-6
Primary Topic
Climate variability and models
Type
article
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article

Multi-model ensemble of CMIP6 projections for past and future climate change on mean precipitation and temperature

Tewodros Getu Engida, Alemayehu Muluneh, Moltot Zewdie
ENVIRONMENTAL SYSTEMS RESEARCH
Climate variability and models
article

Multi-model ensemble of CMIP6 projections for past and future climate change on mean precipitation and temperature

Tewodros Getu Engida, Alemayehu Muluneh, Moltot Zewdie
article en

Abstract

High-resolution climatic Projections are increasingly essential for informed decision-making and efficient adaptation and mitigation planning, especially in climatically sensitive regions such as the Baro River sub-basin in Ethiopia. This study applied station observation data with systematic bias correction utilizing quantile mapping. Historical and future climate trends were analyzed using multi-model ensembles from high-resolution Coupled Model Intercomparison Project phase 6 (CMIP6) under two Shared Socioeconomic Pathways (SSP2-4.5 and SSP5-8.5). The non-parametric Mann–Kendall test and Sen’s Slope estimator were used to detect trends in the 21st century. Historical records (1986–2014) reveal a distinct seasonal rainfall pattern, with peak rainfall occurring in July and August. Projections for the late 21st century (2081–2100) suggest significant increases in mean monthly rainfall by 20.6% (159.1 mm/month) under SSP2-4.5 and by 46.7% (193.5 mm/month) under SSP5-8.5 compared to the historical baseline (132.0 mm/month). Station-level analysis reveals pronounced spatial variability, with substantial increases in rainfall at Lare (+ 129.99%) and Gambella (+ 103.09%) under SSP5-8.5, while other stations show slight increases or even negative trends. Mean annual temperatures are projected to rise by up to 7.16% (reaching 23.69 °C) under SSP2-4.5 and by 18.83% (up to 26.27 °C) under SSP5-8.5, with anomalies reaching as high as 6 °C by the end of the century. Probability density function analysis indicates a shift toward greater variability and more extreme events, mostly under SSP5-8.5. Rainfall distributions exhibit increasing bimodality, while temperature distributions demonstrate widening, indicating a higher likelihood of extreme drought and extreme hot and wet years. These findings emphasize how vulnerable the Baro River Sub-Basin is to hydro-climatic extremes and highlight the urgent need for emissions mitigation and developing strong, tailored adaptation strategies for the area.

ENVIRONMENTAL SYSTEMS RESEARCHVol. 14(1)
Hawassa University (ET), Incell Corporation (United States) (US)
Openalex Percentile: Top 65%
Climate variability and models
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