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The N-ROSS altimeter is an active microwave radiometer, operating in the C band. The relevant instrument parameters are identical to those of the GEOSAT altimeter. The altimeter operates by transmitting a narrow radar pulse. The time of flight, the returned power and the wave shape of the returned pulse are analyzed to provide height of the altimeter above the surface, wind speed, and significant wave height. See Table 3-23 for sensor characteristics. 3. SSM/I. The SSM/I is identical to the DMSP instrument described earlier.
J. , 77,825-842. Blanc, R. , Accuracy of Bulk-method-determined Flux, Stability, and Sea Surface Roughness, 1. Geophys. Res. A. G. Fleagle, 1985: Structure of a cold front over the ocean. Quart. J. R. , 111,739-756. , A Secondary Flow Model for the Planetary Boundary Layer. J. Atmos. Sciences, 27, 742-757, 1970. J. Cardone, T. Guymer, J. E. J. Pierson, S. C. M. Woiceshyn and M. Wurtele; Surface Wind Analyses for SEASAT, J. of Geophys. , 87(C3), 3355-3364, 1982. , and T. Liu, An Operational Large-scale Marine Planetary Boundary Layer Model, J.
J. Mar. , 16, 199-225. , 1986: Wind Forced Internal Waves in the North Pacific and Sargasso Sea. J. Phys. , . , L. Hasse and R. Davis, 1980: Air-Sea Interaction, Instruments and Methods. , 801 pp. , 1978: Whitecaps and Momentum Transfer, in Turbulent Fluxes Through the Sea Surface, Wave Dynamics and Prediction, edited A. Favre and K. Hasselmann, pp. 273-288. , and K. , 1978: Turbulent Fluxes Through the Sea Surface, Wave Dynamics and Prediction. , 665 pp. A. L. H. Stewart, 1981: Anamalous Wind Estimates from the Seasat Scatterometer.