Method and device for detecting supercooled water by utilizing millimeter wave cloud radar and application
A supercooled water and millimeter wave technology, applied in measurement devices, re-radiation, radio wave measurement systems, etc., can solve problems such as inability to detect supercooled water, and achieve the effect of high speed resolution and high spatial and temporal resolution.
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Embodiment 1
[0200] Using the observation data obtained by the Ka-band millimeter-wave cloud radar and microwave radiometer installed in a certain place during the TIPEX-III test, combined with the sounding temperature data of the station, the stratification of a certain day at 22:45-01:00 Supercooled water in clouds is detected using the method of the present invention.
[0201] available:
[0202] as attached Figure 4 The spatio-temporal distribution results of radar parameters of cloud particles in convective clouds detected by millimeter-wave cloud radar are shown, where (a)-(d) are the reflectivity factors Z e , spectral width σ v , Atmospheric vertical velocity V air and the average particle falling velocity From this figure, it can be seen that: from the Z of the global spectrum e According to the echo, the stratocumulus cloud lasted for 2 hours and 15 minutes over the station, the cloud top was about 4.5km high, and the fluctuation was small, but the echo intensity gradient ...
Embodiment 2
[0205] Using the observation data obtained by the Ka-band millimeter-wave cloud radar and microwave radiometer installed in a certain place during the TIPEX-III test, combined with the sounding temperature data of the station, the cumulus congestus on a certain day from 15:45 to 17:30 The supercooled water in cumulus, cumulus and altocumulus is detected using the method of the present invention.
[0206] available:
[0207] as attached Figure 6 The spatio-temporal distribution results of radar parameters of cloud particles in convective clouds detected by millimeter-wave cloud radar are shown, where (a)-(d) are the reflectivity factors Z e , spectral width σ v , Atmospheric vertical velocity V air and the average particle falling velocity It can be seen that from the global spectrum Z e It can be seen that cumulus congestus appeared from 15:50 to 16:40 and lasted for nearly 50 minutes. The cloud layer developed relatively high, and the highest cloud top could exceed 7.5...
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