Abstract
Simultaneous observations of a series of mesocyclonic storms in central Alberta by both C-band Doppler and S-band circular polarization-diversity radars are reported. Attention is focussed on one particular cell which was a right mover. Data show that the circular polarization parameter “degree of polarization” clearly differentiates the storm inflow regions. This suggests that the use of polarization-diversity may be a help in determining storm structure, and therefore an aid in severe storm forecasting.
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