1876.] 



of the Wind and Barometric Pressure. 



409 





O 00 



o o 



+ + 



QC 



o 



+ 



o 



+ + 



CO 



+ 



Oi 



-+-•014 

 + 024 



CO 



+ 



00 



c o 

 + + 



CO 



o 



+ 





1 1 

 + + 



Ol 



+ 







+ 





! T 



cc 



8 



•l 





GC 



o c 







o o 



■l 1 



"i 





o o 



"l 'l 



X 



p 



"l 





c o 

 o o 



"l 1 



a 



1 



o 



CO CO 

 o o 

 o o 



+ 1 



o 

 c 



o 



1 





s 



c 



pa 



c 

 t. 





From M 





OJ 



§ 2 

 o c 



95 



1 



01 

 Ol 



1 1 







oq 



+ 





H i 



+ + 



o 



+ 



o 

 oa 



8 S 



i 

 + 





8 8 

 1 



o 

 p 



*l 





i s 

 1 1 



1 



1 





^ Ol 



o o 



' ■' 



i 





■l 1 



0. 



s 

 1 



lO 



1 1 



O 

 1 





o p 



1 'l 



CO 



oq 

 p 



"l 



CO 



O O 



1 1 



p 

 1 



Ol 



1 1 



CO 



+ 







c 

 c 



c 





£ 

 c 





important peculiarity of fig. 11 appears to be the high morning maximum, 

 •which is higher comparatively than the morning maximum of the actual 



