Abstract

The future planning and management of water resources ought to be based on climate change projections at relevant temporal and spatial scales. This work uses the new regional demarcation for Southern Africa (SA) to investigate the spatio-temporal precipitation variability and trends of centennial-scale observation and modeled data, based on datasets from the sixth phase of the Coupled Model Intercomparison Project (CMIP6). The study employs several statistical methods to rank the models according to their precipitation simulation ability. The Theil–Sen slope estimator is used to assess precipitation trends, with a Student’s t-test for the significance test. The comparison of observation and model historical data enables identification of the best-performing global climate models (GCMs), which are then employed in the projection analysis under two Shared Socioeconomic Pathways (SSPs): SSP2-4.5 and SSP5-8.5. The GCMs adequately capture the annual precipitation variation but with a general overestimation, especially over high-elevation areas. Most of the models fail to capture precipitation over the Lesotho-Eswatini area. The three best-performing GCMs over SA are FGOALS-g3, MPI-ESM1-2-HR and NorESM2-LM. The sub-regions demonstrate that precipitation trends cannot be generalized and that localized studies can provide more accurate findings. Overall, precipitation in the wet and dry seasons shows an initial increase during the near future over western and eastern SA, followed by a reduction in precipitation during the mid- and far future under both projection scenarios. Madagascar is expected to experience a decrease in precipitation amount throughout the twenty-first century.

Highlights

  • Understanding shifts in precipitation variability is crucial for explaining the hydrological cycle response to a natural or forced change in the climate system

  • A disparity in precipitation could heavily impact Southern Africa (SA), where the agricultural sector is a primary source of livelihood

  • By using the new regional demarcations for SA, this study investigates the changes in precipitation variability and trends during the twentieth and twenty-first centuries

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Summary

Introduction

Southern Africa (SA) is one of the regions that are very vulnerable to the effects of climate variability and change. The region has experienced large climatic fluctuations during the past century, with distinct variability at different time scales [4,5]. According to Barros et al [6], SA is highly susceptible to climate change due to its large population, small adaptive ability, poor economic conditions and high exposure. Precipitation over this region is highly variable due to its varying topography and large longitudinal and latitudinal span [7,8,9]. The precipitation trend over SA is complex since the area is bordered by the Atlantic and Indian Oceans to the west and east, respectively [10,11,12]

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