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Old 8th July 2004 | 13:16
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Old Smokey
 
Joined: Jun 2004
Posts: 1,843
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From: Australia
Weather radar wavelength is optimised to detect water droplets. Hence, detection of ice particles, volcanic dust etc. is very weak.

A day to day practical example of this is cruising at high levels but below Cumulo Nimbus tops, looking straight ahead at the Cb shows negligible return (ice crystals only), but tilt down of the radar to 'see' the water droplets is necessary to detect the presence of the Cb.
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