Key Laboratory of Meteorological Disaster of Ministry of Education (KLME), Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and Technology, Nanjing, China; Rwanda Meteorology Agency, Nyarugenge KN 96 St, Kigali, Rwanda; African Institute for Mathematical Sciences Next Einstein Initiative (AIMS-NEI), KG590 St, Kigali, Rwanda.
Key Laboratory of Meteorological Disaster of Ministry of Education (KLME), Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and Technology, Nanjing, China.
Sci Total Environ. 2021 Oct 10;790:148162. doi: 10.1016/j.scitotenv.2021.148162. Epub 2021 May 31.
Previous studies warned that heat extremes are likely to intensify and frequently occur in the future due to climate change. Apart from changing climate, the population's size and distribution contribute to the total changes in the population exposed to heat extremes. The present study uses the ensemble mean of global climate models from the Coupled Model Inter-comparison Project Phase six (CMIP6) and population projection to assess the future changes in high-temperature extremes and exposure to the population by the middle of this century (2041-2060) in Africa compared to the recent climate taken from 1991 to 2010. Two Shared Socioeconomic Pathways (SSPs), namely SSP2-4.5 and SSP5-8.5, are used. Changes in population exposure and its contributors are quantified at continental and for various sub-regions. The intensity of high-temperature extremes is anticipated to escalate between 0.25 to 1.8 °C and 0.6 to 4 °C under SSP2-4.5 and SSP5-8.5, respectively, with Sahara and West Southern Africa projected to warm faster than the rest of the regions. On average, warm days' frequency is also expected to upsurge under SSP2-4.5 (26-59%) and SSP5-8.5 (30-69%) relative to the recent climate. By the mid-21st century, continental population exposure is expected to upsurge by 25% (28%) of the reference period under SSP2-4.5|SSP2 (SSP5-8.5|SSP5). The highest increase in exposure is expected in most parts of West Africa (WAF), followed by East Africa. The projected changes in continental exposure (353.6 million person-days under SSP2-4.5|SSP2 and ~401.4 million person-days under SSP5-8.5|SSP5) are mainly due to the interaction effect. However, the climate's influence is more than the population, especially for WAF, South-East Africa and East Southern Africa. The study findings are vital for climate change adaptation.
先前的研究警告称,由于气候变化,未来极端高温天气很可能会加剧并频繁出现。除了气候变化,人口规模和分布也是导致暴露于极端高温天气的总人口发生变化的原因。本研究使用耦合模式比较计划第六阶段(CMIP6)的全球气候模式集合平均值和人口预测,来评估与 1991 年至 2010 年的近期气候相比,本世纪中叶(2041-2060 年)非洲的高温极端天气变化和人口暴露情况。本研究使用了两种共享社会经济途径(SSP),即 SSP2-4.5 和 SSP5-8.5。在整个非洲大陆和各个次区域量化了人口暴露及其贡献者的变化。在 SSP2-4.5 和 SSP5-8.5 下,高温极端天气的强度预计分别上升 0.25 至 1.8°C 和 0.6 至 4°C,撒哈拉和西南非洲的升温速度预计快于其他地区。平均而言,在 SSP2-4.5(26-59%)和 SSP5-8.5(30-69%)下,温暖日的频率预计也会比近期气候上升。到 21 世纪中叶,在 SSP2-4.5(SSP2)下,人口暴露预计将比参考期增加约 25%(28%);在 SSP5-8.5(SSP5)下,人口暴露预计将增加约 35360 万人/天。在 SSP2-4.5|SSP2 下,人口暴露的增加幅度最大,其次是在 SSP5-8.5|SSP5 下。在 SSP2-4.5|SSP2 下,人口暴露的增加幅度最大,其次是在 SSP5-8.5|SSP5 下。人口暴露的增加主要是由于相互作用的影响。然而,气候的影响超过了人口的影响,尤其是在西非、东南非和东南非。这些研究结果对于气候变化适应至关重要。