SECT. 2] 



LARGE-SCALE INTERACTIONS 



229 



Fig. 63. Diurnal march oiQg, the sensible heat flux from sea to air, in cal cm~2 per day as 

 computed from transfer formula (20) from ship's deck level data taken during 

 Crawford equatorial Atlantic cruise. (After Garstang, 1958, unpublished.) 



Fig. 64. Diurnal march of air temperature (°F) and relative humidity (%) at ship's deck 

 level during Crawford equatorial Atlantic cruise. Note inverse relationship. (After 

 Garstang, 1958, unpublished.) 



