D. Zrnic, N. Balakrishnan, A. Ryzhkov, S. L. Durden
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Use of co-polar correlation coefficient for probing precipitation along the vertical
Presents observations of the co-polar correlation coefficient |/spl rhosub hv/(0)| made with a ground based and airborne weather radars along the vertical. Also differential phase and differential reflectivity at a 10/spl deg/ off nadir are shown. Simple models of prolate and oblate spheroids are used to qualitatively explain the observations.<>