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Paquita Zuidema, Chris Fairall, Leslie M. Hartten, Jeffrey E. Hare, and Daniel Wolfe

few kilometers at 60- and 110-m resolution, even in the absence of precipitation and below cloud base, by virtue of clear-air refractive index Bragg scattering. Details on motion stabilization and processing of the wind profiler data are given in Fairall et al. (1997) . Oceanic temperature and salinity profiles were gathered four times a day to 150-m depth by a conductivity–temperature–depth probe; this probe failed on 31 July. The ocean temperature was measured continuously at 5-cm depth. 3

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Kingtse C. Mo, Eric Rogers, Wesley Ebisuzaki, R. Wayne Higgins, J. Woollen, and M. L. Carrera

adaptive observations. J. Atmos. Sci. , 55 , 633 – 653 . Ripa , P. , and S. G. Marinone , 1989 : Seasonal variability of temperature, salinity, velocity, vorticity and sea level in the central Gulf of California as inferred from historical data. Quart. J. Roy. Meteor. Soc. , 115 , 887 – 913 . Rogers , E. , T. L. Black , D. G. Deaven , G. J. DiMego , Q. Zhao , M. Baldwin , N. W. Junker , and Y. Lin , 1996 : Changes to the operational “early” Eta analysis

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