Method for forecasting growth and hail reduction stages of hail embryos in hail violence process under complex terrain
A complex terrain and stage technology, applied in the forecast field of growth and hailfall stages, can solve the problems of the formation stage of few hail embryos, the forecast indication of the formation stage of few hail embryos, and the inability to obtain quantitative characteristic forecast indicators of hail clouds, etc.
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experiment example 1
[0084] The hailstorm process of experimental example 1 occurred on March 30, 2018. The whole process lasted for 34 minutes. The strongest echo was 61.6dBZ. The area with a large value greater than 55dBZ and hail fell, and moved out of Weining at 17:29.
[0085] like image 3 As shown in a, it is the time of 16:44 in the experimental example 1, and the time of 16:49 is as follows figure 2 As shown in middle b, the height of the echo top increases rapidly from 5km to more than 6km, and the maximum reflectivity reaches 54.2dBZ. After interpolating the corresponding height layer of the temperature layer in the sounding data at 20:00 on the same day, it can be obtained that the 0°C height layer is 4.1km, and the -20°C height layer is 7.3km, that is, the thickness H of the 0°C to -20°C height layer S It is 3.2km, so it meets the requirements of the selected example in this embodiment.
[0086] like Figure 4 As shown in the figure, the variation ratio of supercooled water, the ...
experiment example 2
[0088] The hailstorm process of experimental example 2 occurred on May 18, 2018. The whole process lasted for 60 minutes. The strongest echo was 67.2dBZ. The squall line system was generated in Weining Shuanglong. At this time, a large value area greater than 55dBZ appeared in the monomer, and the hail began to fall at 17:03, and entered the dissipation stage at 17:41.
[0089] like Figure 7 As shown in a, it is the time of 16:48 of the experimental example 2, and the time of 16:54 is as follows Figure 7 As shown in b, the height of the echo top increases rapidly from 9km to more than 10km, and the maximum reflectivity reaches 61.8dBZ. After interpolating the height layer corresponding to the temperature layer in the sounding data at 20:00 on the same day, it can be obtained that the 0°C height layer is 5.2km, and the -20°C height layer is 8.3km, that is, the thickness H of the 0°C to -20°C height layer S It is 3.1km, so it meets the requirements of the selected example in...
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