the thermal capacity between ship and sea. The sea is a large thermal reser- 

 voir, while the ship with its lower thermal capacity will have a lower temper- 

 ature than the temperature over the ocean, as will the air immediately adjacent 

 to and above the ship. 



7 . ACKNOWLEDGMENTS 



The author is most grateful to Harold L. Crutcher and James A. Almazan 

 for their careful review of the manuscript. 



8. REFERENCES 



Almazan, James A., "The Spectrum of Atmospheric Turbulence for Horizontal 



Velocity Components in the Surface Bouncary Layer of a Sea Breeze Cir- 

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 of Texas, Austin, Tex., 1970. 



Brooks, C.E.P., and Carruthers, N., Handbook of Statistical Methods in 

 Meteorology , Her Majesty's Stationery Office, London, 1953. 



Chiu, Wan-Cheng, "The Wind and Temperature Spectra of the Upper Troposphere 

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Malkus, J.S., "On the Structure of the Trade Wind Moist Layer," Papers in 

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Siegel, Sidney, Nonparametric Statistics for the Behavioral Sciences , 

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Yamane, Toro, Statistics, An Introductory Analysis , Harper and Row, 

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