Table VII 



Dally heat totals (go cal , cmT2) lost 

 to the ocean, due to exchange with the 

 atmosphere, for the period 20r27 April 

 1951. 



(3) Convection (see Sec. I4. above) 



Tp(z) now must be adjusted to take care of the total 

 heat, Qq, lost to the ocean as computed above. Since figure 

 7 is plotted in °F. and meters, it is necessary to employ 

 equation (15) in this computation. Substituting for Qg the 

 total given above and solving for the Integral, i-ro obtain 



2322 

 55.6 X.93 



h 



= [[t, {Z)-T{h)]dz = 44.92 T meters (13 ) 



29 



