Changes in the risk of extreme temperatures in megacities worldwide

被引:18
作者
Rajulapati, Chandra Rupa [1 ,2 ,3 ]
Abdelmoaty, Hebatallah Mohamed [4 ,5 ]
Nerantzaki, Sofia D. [3 ,4 ]
Papalexiou, Simon Michael [3 ,4 ,6 ,7 ]
机构
[1] Univ Saskatchewan, Ctr Hydrol, Saskatoon, SK, Canada
[2] Univ Saskatchewan, Ctr Hydrol, Canmore, AB, Canada
[3] Univ Saskatchewan, Global Inst Water Secur, Saskatoon, SK, Canada
[4] Univ Saskatchewan, Dept Civil Geol & Environm Engn, Saskatoon, SK, Canada
[5] Cairo Univ, Fac Engn, Dept Irrigat & Hydraul Engn, Giza, Egypt
[6] Univ Calgary, Dept Civil Engn, Calgary, AB, Canada
[7] Czech Univ Life Sci, Fac Environm Sci, Prague, Czech Republic
基金
加拿大自然科学与工程研究理事会;
关键词
Temperature trends; CMIP6; projections; ETCCDI indices; Heatwaves; Extreme temperature; Megacities; CLIMATE-CHANGE; BIAS CORRECTION; INDEXES; TRENDS; PRECIPITATION; MODEL; SIMULATIONS; IMPACTS; URBANIZATION; EXPANSION;
D O I
10.1016/j.crm.2022.100433
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Globally, extreme temperatures have severe impacts on the economy, human health, food and water security, and ecosystems. Mortality rates have been increased due to heatwaves in several regions. Specifically, megacities have high impacts with the increasing temperature and everexpanding urban areas; it is important to understand extreme temperature changes in terms of duration, magnitude, and frequency for future risk management and disaster mitigation. Here we framed a novel Semi-Parametric quantile mapping method to bias-correct the CMIP6 minimum and maximum temperature projections for 199 megacities worldwide. The changes in maximum and minimum temperature are quantified in terms of climate indices (ETCCDI and HDWI) for the four Shared Socioeconomic Pathways (SSP1-2.6, SSP2-4.5, SSP3-7.0, and SSP5-8.5). Cities in northern Asia and northern North America (Kazan, Samara, Heihe, Montre ' al, Edmonton, and Moscow) are warming at a higher rate compared to the other regions. There is an increasing and decreasing trend for the warm and cold extremes respectively. Heatwaves increase exponentially in the future with the increase in warming, that is, from SSP1-2.6 to SSP5-8.5. Among the CMIP6 models, a huge variability is observed, and this further increases as the warming increases. All climate indices have steep slopes for the far future (2066-2100) compared to the near future (2031-2065). Yet the variability among CMIP6 models in near future is high compared to the far future for cold indices.
引用
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页数:14
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