(319) 



of the wind, the numbers <>t' Table IV have been arranged in 

 Table VI to five groups where as much as possible comparable series 

 have been added together. 



TABLE VI. 



Frequencies deduced from Table IV. 



The comparatively low temperatures for WNW — NNE winds with 

 a small factor of consistency (great distribution) in contrast to the 

 high temperatures and small distribution for WSW — W winds i> 

 very clear from this table. 



At the same time is evident from these data how the combination 

 of series with different mean values decreases the obliquity in the 

 total, so that we can expect that the obliquity factor D, will In- 

 considerably smaller for the total series than D s , calculated lor the 

 various series, which is confirmed by the following table. 



