A globally consistent local-scale assessment of future tropical cyclone risk

被引:77
作者
Bloemendaal, Nadia [1 ]
de Moel, Hans [1 ]
Martinez, Andrew B. [2 ,3 ]
Muis, Sanne [1 ,4 ]
Haigh, Ivan D. [5 ]
van der Wiel, Karin [6 ]
Haarsma, Reindert J. [6 ]
Ward, Philip J. [1 ]
Roberts, Malcolm J. [7 ]
Dullaart, Job C. M. [1 ]
Aerts, Jeroen C. J. H. [1 ]
机构
[1] Vrije Univ Amsterdam, Inst Environm Studies IVM, NL-1081 HV Amsterdam, Netherlands
[2] US Dept Treasury, Off Macroecon Anal, 1500 Penn Ave NW, Washington, DC 20220 USA
[3] Univ Oxford Nuffield Coll, Climate Econometr, Oxford OX1 1NF, England
[4] Deltares, NL-2600 MH Delft, Netherlands
[5] Univ Southampton, Natl Oceanog Ctr, Sch Ocean & Earth Sci, European Way, Southampton SO14 3ZH, Hants, England
[6] Royal Netherlands Meteorol Inst KNMI, NL-3731 GA De Bilt, Netherlands
[7] Met Off, Exeter, Devon, England
基金
欧洲研究理事会; 欧盟地平线“2020”;
关键词
MODEL; RESOLUTION; WIND; INTENSITY;
D O I
10.1126/sciadv.abm8438
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
There is considerable uncertainty surrounding future changes in tropical cyclone (TC) frequency and intensity, particularly at local scales. This uncertainty complicates risk assessments and implementation of risk mitigation strategies. We present a novel approach to overcome this problem, using the statistical model STORM to generate 10,000 years of synthetic TCs under past (1980-2017) and future climate (SSP585; 2015-2050) conditions from an ensemble of four high-resolution climate models. We then derive high-resolution (10-km) wind speed return period maps up to 1000 years to assess local-scale changes in wind speed probabilities. Our results indicate that the probability of intense TCs, on average, more than doubles in all regions except for the Bay of Bengal and the Gulf of Mexico. Our unique and innovative methodology enables globally consistent comparison of TC risk in both time and space and can be easily adapted to accommodate alternative climate scenarios and time periods.
引用
收藏
页数:13
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