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Elizabeth J. Thompson, Steven A. Rutledge, Brenda Dolan, Merhala Thurai, and V. Chandrasekar

-Rayleigh scattering effects ( BC01 ). It also remains unclear whether any of the dual-polarization R relationships require convective/stratiform (C/S) partitioning. Evidence shows that separate R ( z ) equations fit to stratiform and convective rain over tropical oceans improve radar rainfall estimation there ( T15 ). Dual-polarization R relationships with Z dr , K dp , and A h are thought to implicitly account for C/S DSD variability better than Z h alone ( BC01 ; Ryzhkov et al. 2005b ). However, an

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