Analysis of the Dynamic Process of Tornado Formation on 28 July 2024

• Published in: Remote sensing (Basel, Switzerland) Vol. 17; no. 15; p. 2615
• Main Authors: Zhou, Xin, Yang, Ling, Ma, Shuqing, Wang, Ruifeng, Li, Zhaoming, Song, Yuchen, Gao, Yongsheng, Xu, Jinyan
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01.08.2025
• Subjects: 20th century; 21st century; Cyclones; Doppler effect; Doppler radar; dynamic characteristics; Life cycles; Radar arrays; Satellites; Storms; Superhigh frequencies; Thermodynamics; three-dimensional flow field; tornado; Tornadoes; Vortices; Vorticity; Wind; Wind shear; X-band phased burst weather radar; United States > US; China; Guangdong China
• ISSN: 2072-4292; 2072-4292
• DOI: 10.3390/rs17152615

An EF1 tornado struck Nansha District, Guangzhou, Guangdong, on 28 July 2024. To explore the dynamic and thermodynamic changes during the tornado’s life cycle, high-resolution spatiotemporal data from Foshan’s X-band phased-array radar and the direct wind field synthesis algorithm were used to reconstruct the 3D wind field. The dynamics and 3D structure of the tornado were analysed, with a new parameter, vorticity volume (VV), introduced to study its variation. The observation results indicate that the tornado moved roughly from south to north. During the tornado’s early stage (00:10–00:20 UTC), arc-shaped and annular echoes emerged and positive vorticity increased (peaking at 0.042 s−1). Based on the tornado’s movement direction, the right side of the vortex centre was divergent, while the left side was convergent, whereas the vorticity area and volume continued to grow centrally. During the mature stage (00:23–00:25 UTC), the echo intensity weakened and, at 00:24, the vorticity reached its peak and touched the ground, with the vorticity area and volume also reaching their peaks at the same time. During the dissipation stage (00:25–00:30 UTC), the vorticity and echo features faded and the vorticity area and volume also declined rapidly. The analysis showed that the vorticity volume effectively reflects the tornado’s life cycle, enhancing the understanding of the dynamic and thermodynamic processes during the tornado’s development.