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Identifying Multiple Peaks in W-band Radar Doppler Spectra during Drizzle Events in VOCALS 2008 Christopher R. Williams (1, 2), Chris Fairall (2), and Ken Moran (1, 2) (1) CIRES, (2) NOAA ESRL PSD During the VOCALS 2008 cruise, a NOAA W-band (94 GHz) radar was mounted on a stabilized platform and pointed vertically to observe the marine boundary layer cloud structure. Occasionally during drizzle events, while the reflectivity was consistent with time and height, the estimated spectrum width had large values. Examination of the Doppler velocity power spectra reveled that many of the spectra with large spectrum widths actually contained multiple peaked spectra. These multiple peak spectrum invalidates the assumption that drizzle can be modeled as a single peaked spectrum of droplets described by three parameters (e.g., intensity, mode, and spread). The observed multiple peaked spectra suggest that multiple physical processes are generating different sized drizzle droplets that are being observed within the same radar pulse volume. |

