China News Service, Guangzhou, March 27 (Wang Jian and Wang Tianwei) The Guangdong Meteorological Bureau reported on the 27th that the province continued to be affected by cold air and shear lines that day, and many parts of the province encountered strong convective weather. Among them, northern Maoming, There were thunderstorms in Yunfu and southern Zhaoqing, local strong thunderstorms, and short-term showers in parts of northern Guangdong, the Pearl River Delta, and eastern Guangdong.
According to meteorological and hydrological monitoring, from 8:00 on the 27th to 17:00 on the 27th, 11 towns and streets in the province recorded heavy rain of more than 25 mm. Among them, Mugang Street, Duanzhou District, Zhaoqing recorded the province's maximum rainfall of 32.2 mm.
The Guangdong Provincial Meteorological Bureau predicts that on the 28th, affected by high-altitude troughs and cold air, the weather in the central and northern parts of the province will be cool in the morning and evening, and there will be moderate thunderstorms and local heavy rains in the southern coastal cities and counties.
From the 29th to the 30th, affected by the high-altitude trough and the low-level south-to-southeast airflow, most of the province turned into warm, humid, rainy and foggy weather, and the temperature rose in various places; there were moderate to heavy rains in the eastern and southern cities and counties, and local torrential rains, and the rest of the cities and counties experienced heavy rains. Thunderstorms are locally heavy rains, accompanied by strong convective weather such as thunder and lightning, short-term strong winds of magnitude 6 to 8, and short-term heavy precipitation.
At the same time, on the 28th, the northeasterly winds of the province's sea surface were 6 to 7 gusts of 8, and the northerly winds of the Beibu Gulf were 6 to 7 gusts of 8 to 6 gusts of 7.
Meteorological experts reminded that Guangdong has entered a season of frequent strong convection and heavy precipitation, and it is necessary to pay attention to the strong convective weather and its secondary disasters such as lightning and short-term strong winds.
In addition, because the precipitation in the early stage of the province has resulted in a lot of soil water content, and the later precipitation areas overlap, it is necessary to guard against heavy precipitation and the resulting geological disasters such as urban and rural waterlogging, mountain torrents, mudslides, and landslides.
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