Abstract

We analyze data of 27 global climate models from the sixth phase of the Coupled Model Intercomparison Project (CMIP6), and examine projected changes in temperature and precipitation over the African continent during the twenty-first century. The temperature and precipitation changes are computed for two future time slices, 2030–2059 (near term) and 2070–2099 (long term), relative to the present climate (1981–2010), for the entire African continent and its eight subregions. The CMIP6 multi-model ensemble projected a continuous and significant increase in the mean annual temperature over all of Africa and its eight subregions during the twenty-first century. The mean annual temperature over Africa for the near (long)-term period is projected to increase by 1.2 °C (1.4 °C), 1.5 °C (2.3 °C), and 1.8 °C (4.4 °C) under the Shared Socioeconomic Pathways (SSPs) for weak, moderate, and strong forcing, referenced as SSP1-2.6, SSP2-4.5, and SSP5-8.5, respectively. The future warming is not uniform over Africa and varies regionally. By the end of the twenty-first century, the largest rise in mean annual temperature (5.6 °C) is projected over the Sahara, while the smallest rise (3.5 °C) is over Central East Africa, under the strong forcing SSP5-8.5 scenario. The projected boreal winter and summer temperature patterns for the twenty-first century show spatial distributions similar to the annual patterns. Uncertainty associated with projected temperature over Africa and its eight subregions increases with time and reaches a maximum by the end of the twenty-first century. On the other hand, the precipitation projections over Africa during the twenty-first century show large spatial variability and seasonal dependency. The northern and southern parts of Africa show a reduction in precipitation, while the central parts of Africa show an increase, in future climates under the three reference scenarios. For the near (long)-term periods, the area-averaged precipitation over Africa is projected to increase by 6.2 (4.8)%, 6.8 (8.5)%, and 9.5 (15.2)% under SSP1-2.6, SSP2-4.5, and SSP5-8.5, respectively. The median warming simulated by the CMIP6 model ensemble remains higher than the CMIP5 ensemble over most of Africa, reaching as high as 2.5 °C over some regions, while precipitation shows a mixed spatial pattern.

Highlights

  • Africa, the second most populous continent in the world, is one of the regions most vulnerable to climate change due to its high exposure and low adaptive capacity (Sutton et al 2011; Barros et al 2014)

  • We analyzed a multi-model ensemble based on 27 CMIP6 models and examined projected temperature and precipitation changes over Africa in the twenty-first century

  • These changes were computed for the African continent and its eight subregions during two future time slices (2030–2059 and 2070–2099) relative to the present climate (1981–2010)

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Summary

Introduction

The second most populous continent in the world, is one of the regions most vulnerable to climate change due to its high exposure and low adaptive capacity (Sutton et al 2011; Barros et al 2014). Barkhordarian et al (2012) found an increasing trend in the observed annual and seasonal mean surface temperatures over North Africa. Anyah and Qiu (2012) observed an increase in temperature over the southern and eastern parts of Africa in recent decades. According to IPCC AR5, mean annual precipitation decreased over the western and eastern Sahel regions in northern Africa, while it increased over parts of eastern and southern Africa, in the past century (IPCC 2013). The overall reduction in seasonal and annual precipitation over different parts of the African continent during the twentieth century is noted by several other studies (Sylla et al 2016, 2018; Klutse et al 2018) (Hoerling et al 2006; Lebel and Ali 2009; Lyon and Dewitt 2012; Mohamed 2011; New et al 2006). This paper further describes projected annual and seasonal mean changes in temperature and precipitation over eight African subregions (described )

Data and Methodology
27 UKESM1-0-LL
Observed Climatology and Climate Models’ Evaluation
Projected Changes in Temperature and Precipitation During the Boreal Winter
Differences Between CMIP5‐ and CMIP6‐Projected Signals Over Africa
Summary and Conclusions
Full Text
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