'. Loomis — Results fror 



pretty well repre- 



and the summer oscillations by the formula : 



S= l-000sin2Z + 0.104 cos^Z. 

 The differences between the observed and computed values a 



! Atlantic Ocean by Maury's Charts. 



_ ! 



I 



j 



601103 



lit 





Tj11S?1|S'^ 



16371.™ 



"s''i1" 





Vi sj 11 10 10 1= 15} 1, 



rs*^ 



111 





243 419312974 1797 1393 1100 773 48oi 349 % 



111 



^ 34^ 334 2 





1534 2265 1645 766 723 860 986 8931 747 3 



g "t '1 



1 ^ ' 





lOJJl^US. »g .05 3.15. 



lr 



6 S i 





IT 



ill 



^ 





riTi|iTii1|t 



•ni 



i i 





iidrnl# 



*^i^- 



1 i 





11 rrrrr'T'rr ;i 1: 



'ol 





