Abstract

Weather and climate extremes, such as heat waves (HWs), have become more frequent due to climate change, resulting in negative environmental and socioeconomic impacts in many regions of the world. The high vulnerability of South African society to the impacts of warm extreme temperatures makes the study of the effect of climate change on future HWs necessary across the country. We investigated the projected effect of climate change on future of South Africa with a focus on HWs using an ensemble of regional climate model downscalings obtained from the Conformal Cubic Atmospheric Model (CCAM) for the periods 2010–2039, 2040–2069, and 2070–2099, with 1983–2012 as the historical baseline. Simulations were performed under the Representative Concentration Pathway (RCP) 4.5 (moderate greenhouse gas (GHG) concentration) and 8.5 (high GHG concentration) greenhouse gas emission scenarios. We found that the 30-year period average maximum temperatures may rise by up to 6 °C across much of the interior of South Africa by 2070–2099 with respect to 1983–2012, under a high GHG concentration. Simulated HW thresholds for all ensemble members were similar and spatially consistent with observed HW thresholds. Under a high GHG concentration, short lasting HWs (average of 3–4 days) along the coastal areas are expected to increase in frequency in the future climate, however the coasts will continue to experience HWs of relatively shorter duration compared to the interior regions. HWs lasting for shorter duration are expected to be more frequent when compared to HWs of longer durations (over two weeks). The north-western part of South Africa is expected to have the most drastic increase in HWs occurrences across the country. Whilst the central interior is not projected to experience pronounced increases in HW frequency, HWs across this region are expected to last longer under future climate change. Consistent patterns of change are projected for HWs under moderate GHG concentrations, but the changes are smaller in amplitude. Increases in HW frequency and duration across South Africa may have significant impacts on human health, economic activities, and livelihoods in vulnerable communities.

Highlights

  • Characteristics of extreme temperature events are expected to change due to global warming/global mean temperature increases

  • Under a high greenhouse gas (GHG) concentration, short lasting heat waves (HWs) along the coastal areas are expected to increase in frequency in the future climate, the coasts will continue to experience HWs of relatively shorter duration compared to the interior regions

  • The HW thresholds are generally higher across the western parts of the country, ranging from 32 to 44 °C, in line higher across the western parts of the country, ranging from 32 to 44 ◦ C, in line with observed average temperatures shown in Figure 2a during DJF

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Summary

Introduction

Characteristics of extreme temperature events are expected to change due to global warming/global mean temperature increases. The impacts of HWs on agriculture, the economy, and on human beings, and the high vulnerability of South African society to the impacts of extremely warm temperatures highlight the necessity to study the occurrence and nature of these events and their projected changes. It has been indicated that health and climate change adaptation strategy discussions are often limited in South African sub-national governments [28] This can partially be credited to the lack of research of other extreme events such as HWs. In depth knowledge about the projections of HWs in. Previous studies (e.g., [15]) have indicated that regional climate models project an increase in duration, frequency, and intensity of extreme events for the 21st century. Comparisons of simulated average maximum temperatures, HW thresholds, and variability are presented in relation to observations followed by HWs in future warmer climates and concluding remarks

Data and Methods
Results
C inthe thecoastal
45 HWs from to1983
Period 2010 to 2039
Period
Period 2040 to 2069
Period 2070 to 2099
Summary and Conclusions
Full Text
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