Here l+ij-.^H Is the number of squarasj bounded by one meter and 

 one °P., which must be subtracted graphically from Tp(z) to 

 arrive at the predicted temperature distribution. This is done 

 in figure 8, ana the resulting distribution is Tp(z)o 



TEMPERATURE (T) 



62 63 64 65 66 67 68 6= 70 



72 73 74 75 76 77 78 79 80 



10 



12 

 in 



£ 14 

 u 

 S .6 



X 



I- 



Si IB 

 o 



20 

 22 



24 

 26 

 26 

 30 



FIGURE 8. CHANGE IN TEMPERATURE DISTRIBUTION DUE TO HEAT EXCHANGE WITH ATMOSPHERE 

 AND DUE TO CONVECTION. 20-27 APRIL 1951 



{I4.) Turbulent mixing (see Sec. 5 above) 



The character of Tq{z) was so unusual that it was 

 considered probable from past experience that the wind and 

 sea would be of enough force to mix the shallow layer in 

 which two abrupt discontinuities are shown. Some of this 

 abruptness undoubtedly is due to the discontinuous manner in 

 which the temperature changes due to radiation must be plotted. 

 Therefore, T (z) xx'as adjusted by graphic means according to the 



30 



