Hu Sheng, Luo Cong, Zhang Yu, et al. Doppler radar features of severe hailstorms in Guangdong Province. J Appl Meteor Sci, 2015, 26(1): 57-65. DOI: 10.11898/1001-7313.20150106.
Citation:
Hu Sheng, Luo Cong, Zhang Yu, et al. Doppler radar features of severe hailstorms in Guangdong Province. J Appl Meteor Sci, 2015, 26(1): 57-65. DOI: 10.11898/1001-7313.20150106.
Hu Sheng, Luo Cong, Zhang Yu, et al. Doppler radar features of severe hailstorms in Guangdong Province. J Appl Meteor Sci, 2015, 26(1): 57-65. DOI: 10.11898/1001-7313.20150106.
Citation:
Hu Sheng, Luo Cong, Zhang Yu, et al. Doppler radar features of severe hailstorms in Guangdong Province. J Appl Meteor Sci, 2015, 26(1): 57-65. DOI: 10.11898/1001-7313.20150106.
Doppler weather radar features of 12 severe hailstorms in Guangdong Province are studied.Firstly, radar echo characteristics including the maximum reflectivity, maximum reflectivityheight, the echo top, 45 dBZ echo height, the vertically integrated liquid (VIL) water, the VIL density and the vertical gradient of reflectivity are calculated. The maximum reflectivity of these 12 hailstorms are mostly over 65 dBZ with the highest value of 73 dBZ. The maximum echo heights are over 5 km with the highest being 9.2 km. Besides, all of 45 dBZ echo heights reach 9.7 km. The maximum VIL is 91 kg·m-2 and only one storm's maximum VIL is less than 50 kg·m-2. The average vertical gradient of reflectivity is 2.4 dB·km-1, and the minimum vertical gradient of reflectivity is 0.5 dB·km-1.Secondly, three body scatter spike (TBSS) features, side-lobe echoes, and reflectivity distribution features in 0℃ and-20℃ environmental temperature layers of 12 sever hailstorms are analyzed. Side-lobe echoes and TBSS features are observed in 3 and 6 hailstorms, respectively, but they are found simultaneously only in one severe hailstorm. Severe hails occur within 0-40 minutes after the first TBSS feather or the side-lobe echo appears, and the average forecast lead time is about 14 minutes. Average heights of the 0℃ and-20℃ environmental temperature layers around 12 severe hailstorms are 4502 m and 7682 m. All the maximum echoes of 12 severe hailstorms in 0℃ and-20℃ layers are over 54 dBZ, and the maximum values are 67 dBZ and 66 dBZ in different layers.Finally, vertical reflectivity profiles between severe hailstorms and non-hail storms are compared. For severe hailstorms, most of the maximum echoes exceed 65 dBZ, and their heights are between 5 km and 10 km. Radar echoes in hailstorms below 10 km are over 40 dBZ, and 30 dBZ echoes can extend to 15 km or higher. For non-hail storms in hailstorm days, the maximum echoes are about 60 dBZ, and corresponding heights are lower, located at 2-5 km levels. 40 dBZ echoes in storms are rarely above 10 km. It shows that these storms in hailstorm days can't generate large hail because of their weaker vertical updraft and weaker, reflectivity. For storms in non-hailstorm days, the maximum echoes vary from 55 dBZ to 68 dBZ, and heights of most of them are about 5 km. 40 dBZ echoes in some storms can extend to 10 km or higher, however, large hails don't occur for these strong storms due to different environmental conditions.
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