( 320 ) 



TABLE VII. 



Constants of the frequency-numbers of Table VI. 



The (negative) obliquity D, is therefore strongest for the northerly 

 seawinds with low temperature and decreases further regularly with 

 the azimuth counted from North through East. The symmetrical 

 deviation I) t is greatest for southerly winds and smallest for calms. 



TABLE VIII. 



Analysis of the frequencies of Table VI. 



O 



o-c 



C 3 



O-Q-C, C 4 ! 0—-ZC 



