TEMPERATURE (°F) 

 62 63 64 65 66 67 68 69 70 7 1 72 73 74 75 76 77 78 79 60 



FIGURE 7. CHANGE IN TEMPERATURE DISTRIBUTION DUE TO RADIATION, 20-27 APRIL 1951. 



resulting temperature distribution is Tp(z), and is shown in 

 figure 7« 



(2) Heat exchange with atmosphere (see Sec. 3 above) 

 It is now necessary to compute the amount of heat 

 gained or lost by the ocean from exchange with the atmosphere. 

 This may be done easily for each day of the forecast period 

 by the use of equation (12) and the meteorological data present- 

 ed in table III. The results of 0,^ for each day are presented 



in table VII. Addition of these daily values of Q gives a 



_p 

 total of 2,322 g. cal. cm. , v/hich is the total heat lost to 



the ocean by exchange with the atmosphere. 



28 



