Substantial Increase in the Joint Occurrence and Human Exposure of Heatwave and High-PM Hazards Over South Asia in the Mid-21st Century

被引:41
作者
Xu, Yangyang [1 ]
Wu, Xiaokang [1 ,2 ]
Kumar, Rajesh [2 ]
Barth, Mary [2 ]
Diao, Chenrui [1 ]
Gao, Meng [3 ]
Lin, Lei [4 ,5 ]
Jones, Bryan [6 ]
Meehl, Gerald A. [2 ]
机构
[1] Texas A&M Univ, Dept Atmospher Sci, College Stn, TX 77843 USA
[2] Natl Ctr Atmospher Res, POB 3000, Boulder, CO 80307 USA
[3] Hong Kong Baptist Univ, Dept Geog, Hong Kong, Peoples R China
[4] Sun Yat Sen Univ, Sch Atmospher Sci, Zhuhai, Guangdong, Peoples R China
[5] Sun Yat Sen Univ, Guangdong Prov Key Lab Climate Change & Nat Disas, Zhuhai, Guangdong, Peoples R China
[6] Baruch Coll, Marxe Sch Publ & Int Affairs, New York, NY USA
来源
AGU ADVANCES | 2020年 / 1卷 / 02期
基金
美国国家科学基金会; 中国国家自然科学基金;
关键词
heat and high-PM hazard; CLIMATE-CHANGE; AIR-POLLUTION; PARTICULATE MATTER; ANTHROPOGENIC INFLUENCE; ATMOSPHERIC CHEMISTRY; PUBLIC-HEALTH; EXTREME HEAT; BLACK CARBON; TEMPERATURE; MORTALITY;
D O I
10.1029/2019AV000103
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Extreme heat occurrence worldwide has increased in the past decades. Greenhouse gas emissions, if not abated aggressively, will lead to large increases in frequency and intensity of heat extremes. At the same time, many cities are facing severe air pollution problems featuring high-PM episodes that last from days to weeks. Based on a high-resolution decadal-long model simulation using a state-of-the-science regional chemistry-climate model that is bias corrected against reanalysis, here we show that when daily average wet-bulb temperature of 25 degrees C is taken as the threshold for severe health impacts, heat extremes frequency averaged over South Asia increases from 45 5 days/year in 1997-2004 to 78 3 days/year in 2046-2054 under RCP8.5 scenario. With daily averaged PM2.5 surface concentration of 60 mu g/m(3) defined as the threshold for such "unhealthy" extremes, high-PM extremes would occur 132 8 days/year in the Decade 2050 under RCP8.5. Even more concerning, due to the potential health impacts of two stressors acting in tandem, is the joint occurrence of the heatwave and high-PM hazard (HHH), which would have substantial increases of 175% in frequency and 79% in duration. This is in contrast to the 73-76% increase for heatwave or high PM when assessed individually. The fraction of land exposed to prolonged HHH increases by more than tenfold in 2050. The alarming increases in just a few decades pose great challenges to adaptation and call for more aggressive mitigation. For example, under a lower emission pathway, the frequency of HHH will only increase by 58% with a lower frequency of high-PM extremes. Plain Language Summary Extreme heat occurrence worldwide has increased in the past decades. At the same time, many cities are facing severe air pollution problems featuring high-PM episodes (high concentration of particulate matter due to various sources) that last from days to weeks. We present an integrated assessment of human exposure to the joint occurrence of the heatwave and high-PM extremes, and possible future changes have been missing. In addition to the expected elevation in the heatwave and high-PM-related extremes, we also show that the rare jointed events would have quite large increases in the future with a 175% increase in frequency. The fraction of land exposed to prolonged HHH would increase by more than tenfold in 2050. The alarming rate of increases in just a few decades pose great challenges to adaptation. Key Points A regional-scale assessment for the present-day heatwave and high-PM occurrence and future changes is presented The rare heatwave and high-PM hazards (HHH) would have large increases, in contrast to smaller increases in heatwave or high PM individually The alarming increase rate in the next few decades poses great challenges to adaptation, calling for a holistic view of the health impacts
引用
收藏
页数:19
相关论文
共 85 条
[1]   Global observed long-term changes in temperature and precipitation extremes: A review of progress and limitations in IPCC assessments and beyond [J].
Alexander, Lisa V. .
WEATHER AND CLIMATE EXTREMES, 2016, 11 :4-16
[2]   Methods to Calculate the Heat Index as an Exposure Metric in Environmental Health Research [J].
Anderson, G. Brooke ;
Bell, Michelle L. ;
Peng, Roger D. .
ENVIRONMENTAL HEALTH PERSPECTIVES, 2013, 121 (10) :1111-1119
[3]  
[Anonymous], 2005, Air quality guidelines - global update 2005
[4]  
[Anonymous], 2020, Notification
[5]   Cooling China: The Weather Dependence of Air Conditioner Adoption [J].
Auffhammer, Maximilian .
FRONTIERS OF ECONOMICS IN CHINA, 2014, 9 (01) :70-84
[6]   Heat-Related Mortality in India: Excess All-Cause Mortality Associated with the 2010 Ahmedabad Heat Wave [J].
Azhar, Gulrez Shah ;
Mavalankar, Dileep ;
Nori-Sarma, Amruta ;
Rajiva, Ajit ;
Dutta, Priya ;
Jaiswal, Anjali ;
Sheffield, Perry ;
Knowlton, Kim ;
Hess, Jeremy J. .
PLOS ONE, 2014, 9 (03)
[7]  
Balakrishnaiah G., 2011, Characterization of PM, PM 10 and PM 2.5 mass concentrations at a tropical semi-arid station in Anantapur
[8]   What measure of temperature is the best predictor of mortality? [J].
Barnett, A. G. ;
Tong, S. ;
Clements, A. C. A. .
ENVIRONMENTAL RESEARCH, 2010, 110 (06) :604-611
[9]   Historical and Projected Surface Temperature over India during the 20th and 21st century [J].
Basha, Ghouse ;
Kishore, P. ;
Ratnam, M. Venkat ;
Jayaraman, A. ;
Kouchak, Amir Agha ;
Ouarda, Taha B. M. J. ;
Velicogna, Isabella .
SCIENTIFIC REPORTS, 2017, 7
[10]   Bias corrections of global models for regional climate simulations of high-impact weather [J].
Bruyere, Cindy L. ;
Done, James M. ;
Holland, Greg J. ;
Fredrick, Sherrie .
CLIMATE DYNAMICS, 2014, 43 (7-8) :1847-1856