The Deadliest Tornado (EF4) in the Past 40 Years in China

Author:

Meng Zhiyong1,Bai Lanqiang1,Zhang Murong1,Wu Zhifang2,Li Zhaohui34,Pu Meijuan5,Zheng Yongguang6,Wang Xiaohua5,Yao Dan7,Xue Ming891011,Zhao Kun89,Li Zhaoming3,Peng Siqi2,Li Liye3

Affiliation:

1. Laboratory for Climate and Ocean–Atmosphere Studies, Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, China

2. Guangdong Meteorological Bureau, Guangdong, China

3. Foshan Tornado Research Center, Guangdong, China

4. Weathernews America Inc., Norman, Oklahoma

5. Jiangsu Meteorological Bureau, Nanjing, China

6. National Meteorological Center, Beijing, China

7. State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing, China

8. Key Laboratory of Mesoscale Severe Weather, Ministry of Education of China, Nanjing University, Nanjing, China

9. School of Atmospheric Sciences, Nanjing University, Nanjing, China

10. Center for Analysis and Prediction of Storms, Oklahoma University, Norman, Oklahoma

11. School of Meteorology, Oklahoma University, Norman, Oklahoma

Abstract

Abstract An EF4 supercellular tornado hit Funing County, Yancheng, Jiangsu Province, China, from about 1410 to 1500 local standard time 23 June 2016, causing 98 fatalities and 846 injuries. It was the deadliest tornado in the past 40 years in China. This paper documents the storm environment, evolution of the radar signatures, real-time operational tornado warning services, and the damage distribution during this event. The tornado was spawned from a supercell that developed ahead of an upper-level trough extending southwestward from a low pressure vortex in northeast China and dissipated following the occlusion of the tornado vortex. The radar-based rotational velocity of the mesocyclone peaked at 42.2 m s−1. The strength of the tornado vortex signature (gate-to-gate azimuthal radial velocity difference) peaked at 84.5 m s−1. Surface observations at 1-min intervals from a mesoscale network of in situ surface weather stations revealed the surface wind pattern associated with the mesocyclone, such as convergent and rotational flows. The tornado formed after the peak updraft strength of the supercell, producing a damage swath that was 34.5 km long and with a maximum width of 4.1 km. The review of the tornado warning process for this event reveals that there is much work to be done to develop operational tornado forecast and warning services for China.

Funder

the National Natural Science Foundation of China

the Ministry of Science and Technology of China

Publisher

American Meteorological Society

Subject

Atmospheric Science

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