Multivariate Analysis and Warning of a Tornado Embedded in Tropical Cyclone in Southern China

An EF1 tornado associated with tropical cyclone (TC) Ewiniar hit Dali Town, Foshan, Guangdong Province at 06:03 UTC on June 8, 2018, and the first special tornado warning was issued to five towns at 05:05 UTC. This article utilizes minute-scale observations from an X-band dual-polarization radar and...

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Autores principales: Zhaoming Li, Haonan Chen, Hongxing Chu, Haobo Tan, V. Chandrasekar, Xianxiang Huang, Shuofu Wang
Formato: article
Lenguaje:EN
Publicado: IEEE 2021
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Acceso en línea:https://doaj.org/article/23ef94caf7714a50a8e5362bc4479ce9
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Sumario:An EF1 tornado associated with tropical cyclone (TC) Ewiniar hit Dali Town, Foshan, Guangdong Province at 06:03 UTC on June 8, 2018, and the first special tornado warning was issued to five towns at 05:05 UTC. This article utilizes minute-scale observations from an X-band dual-polarization radar and measurements from an S-band Doppler radar to resolve the polarization characteristics associated with this tornado. In addition, second-scale atmospheric pressure data obtained from micropressure gauge and NCEP FNL (Final) Operational Global Analysis data are used to investigate the synoptic conditions and features of gravity waves (GWs). The conspicuous features of the descending reflectivity core, Doppler velocity couplet, <italic>Z</italic><inline-formula><tex-math notation="LaTeX">$_{\text{DR}}$</tex-math></inline-formula> arc, <italic>K</italic><inline-formula><tex-math notation="LaTeX">$_{\text{DP}}$</tex-math></inline-formula> foot, and the separation of the <italic>Z</italic><inline-formula><tex-math notation="LaTeX">$_{\text{DR}}$</tex-math></inline-formula> arc and <italic>K</italic><inline-formula><tex-math notation="LaTeX">$_{\text{DP}}$</tex-math></inline-formula> foot are detailed to quantify the tornadic evolution. The amplitude fluctuation of the GWs suddenly increased to 77.3 Pa, 2 h before the tornado occurred. Two focus regions with <italic>K</italic><inline-formula><tex-math notation="LaTeX">$_{\text{DP}}$</tex-math></inline-formula> values greater than 6<inline-formula><tex-math notation="LaTeX">$^\circ$</tex-math></inline-formula>/km are discussed by combining the Doppler velocity couplet and <italic>Z</italic><inline-formula><tex-math notation="LaTeX">$_{\text{DR}}$</tex-math></inline-formula> arc. The separation distance of the <italic>Z</italic><inline-formula><tex-math notation="LaTeX">$_{\text{DR}}$</tex-math></inline-formula> arc and <italic>K</italic><inline-formula><tex-math notation="LaTeX">$_{\text{DP}}$</tex-math></inline-formula> foot was approximately 2.1 km. The appearance of these features may be indicative of fundamental processes intrinsic to tornado storms.