Climate of Victoria. 5 



The relative frequency of the wind is shown in the follow- 

 ing table : — 



a 

















I 



(t 1 





o 



CO 



r~ 



to 



CO 



CO 



<N 



CO 



r~ 



Tf 



CO 



B 























CO 



in 



■<(< 



m 



t. 







-" 



T(- 



Tf 



<N 



c< 



c 





















^ 



CO 



m 





W 



**- 



J 



*» y 



fH 



o 



to 



CO 



CO 



pa 























o 



co 



to 



in 



CO 









-* 



i^ 



lO 



CO 



CO 



a 

















| 



2 a 

 to B 



$ 



1ft 



o 



to 



■* 



<N 



- 



• in 



CO 



~ 



CM 



H 



















^ 





>o 



o 



00 



t^ 



to 





to 





r-1 



to 



■* 



" 



CM 



s 







m 















to 



<N 



00 



OS 



cm 



in 





to e 



1-1 



OS 



in 



cm 



CO 



M 























o 



CM 



<N 



^ 



»n 





to 





CO 



OS 



to 



<M 



o 



s 

















1 







to 



o 



■* 



*>. 



m 



^ § 



to 



CO 



£ 



to 



CM 



m 



M 



















H 





rl 



Tt> 



to 



CM 



CO 





to 





CO 



£ 



T)< 



CO 



tH 



c 

















CJ 



_j 



to" 



in 



00 



CO 



en 



C5 





« g 



>H 



CM 



c< 



r- 



i-l 



« 























O 



CM 



o 



o 



O 





H 















P 

















l 



as ca 



H 



« 



o 



00 



CM 



to 



S) 























en 



a> 



00 



to 



T)< 





to 





rt 



1-1 



co 



C] 



<N 



a 

















I 



-a 





CO 



i^ 



o 



1— 1 



p— L 



73 § 



oi 



CM 



■-H 



in 



■* 



co 



n 























t~ 



as 



00 



<N 



CO 





05 





<M 



CO 



*~ 



in 



•* 









S>> 



fee 



fc»" 



' 

















/= 











S 



«1 



fc 



a> 











h 



fe. 



a 















<! 



1-5 



O 



1-5 













c 

 l-s 



CO 







H 



■ c3 



>2 



