Data processing method for forecasting heavy precipitation weather
A data processing and heavy precipitation technology, applied in the direction of electrical digital data processing, special data processing applications, instruments, etc., can solve the problems such as difficult to realize automatic objective analysis, difficult to accurately describe numerical models, and large deviations in weather phenomenon forecasting
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Embodiment 1
[0068] Example 1 Precipitation in northern Henan in August 2009
[0069] On August 17, 2009, heavy precipitation occurred in the north-central part of Henan Province and the west part of Shandong Province ( figure 1 ), the maximum precipitation reached 176mm from 00:00 on the 17th to 00:00 on the 18th (UTC, the same below), and the heavy precipitation was mainly concentrated at 00-12:00. On the weather map at 500hPa at 12:00 on August 16, the Asian continent north of 45°N showed two troughs and two ridges (figure omitted); south of 45°N, there was a wide low trough in the Hetao area of my country, and Moving eastward, the western ridge point of the subtropical high in the western Pacific is located at about 100°E, and the eastern part of my country is under the control of the southerly airflow. From 00 to 06 on the 17th, the western Pacific subtropical high was basically stable in the East China region, the eastward movement of the Hetao low trough slowed down, and the North...
Embodiment 22012
[0079] Example 2 Extreme precipitation in Beijing area on July 21, 2012
[0080] In order to further verify the application of the method of the present invention in extreme precipitation, the historically rare torrential rain that occurred in Beijing and parts of Hebei Province on July 21, 2012 was analyzed. The average rainfall in Beijing is 164mm, which is the largest in 61 years. This rainstorm occurred under the circulation situation of the north vortex and the south trough, high in the east and low in the west. The heavy rainfall area is located on the right rear side of the entrance area of the high-altitude jet, and the high-altitude 200hPa is a significant diversion area (figure omitted); There is a high-altitude trough around the Hetao area, and the Beijing area is located in front of the trough. In fact, this precipitation has two phases: from 02 to 08:00 on July 21, it is the precipitation phase in the warm area, dominated by stratiform clouds, and the precipita...
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