LIST OP TABLES 



Table I 

 Table II 



Table III 

 Table IV 



Table V 



Table VI 



Table VII 



Table VIII 



Table IX 



Table X 



Table XI 

 Table XII 



Typical daily temperature changes {°F) due 

 to the absorption of radiation at various 

 latitudes and depth intervals. 



Amount of heat (g. cal. cmr^ dayT ) that 

 is lost to the ocean due to exchange with the 

 atmosphere for various wind speeds and sea-air 

 temperature differences. 



Mean daily values of various meteorological 

 parameters for 20-27 April 1951. 



and back radiation (g. cal. cra."'^ min. "■*■) 



Computed and measured rates of tqtal incoming 

 and back radiation (g 

 for 20-27 April 1951. 



Total heat (g. cal. cm,"'^) that is added 

 to each layer of the water column because of 

 absorption of radiation in the red and other 

 spectral bands during the period 20-27 April 

 1951. 



Temperature changes in the various layers due 

 to the absorption of radiation during the 

 period 20-27 April 1951. 



— 2 

 Daily heat total (g. cal. cm. ) lost to the 



ocean, due to exchange with the atmosphere, 



for the period 20-27 April 1951. 



Fourier coefficients as computed from anchor 

 station of k Dec. 1950. 



Relative amplitudes, w, as computed from anchor 

 station of l^. Dec. 1950. 



Relative amplitudes, w, as computed from single 

 density distribution on 9 Dec. 1950. 



Predicted Foorier coefficients for 9 Dec. 1950. 



Predicted and observed absolute amplitudes 

 (meters) of the diurnal internal wave on 

 9 Dec. 1950. 



Xlll 



