( 318 ) 



More clearly than in the numbers of Table IV does the influence 

 tit' the direction of the wind on the temperature show itself in I lie 

 mean temperature M and the factor of consistency h, arranged in 

 Table V. 



TABLE V. 



Direction Number M ->n 

 of wind ; of I Temp V 

 Magn. ; observ. j ' emp - M ' 



N 



NNE 



NE 



ENE 



E 



ESE 



SE 



SSE 



S 



SSW 



SW 



wsw 

 w 



WNW 

 NW 

 NNW 

 Calm 



349 

 258 

 375 

 191 

 185 



95 

 130 



77 

 124 

 125 

 337 

 656 

 585 

 272 

 311 

 264 

 182 



13.10 

 16.33 



17.50 

 17.61 

 17.68 

 17.53 

 17 77 

 17.07 

 17.39 

 17.38 

 17.23 

 17.08 

 17.10 

 16.32 

 16.27 

 15 65 

 18.56 



0.3485 

 0.3478 

 0.3477 

 0.3561 

 0.3155 

 3401 

 0.3527 

 0.3436 

 0.3713 

 0.3754 

 0.4037 

 0.5121 

 0.4685 

 I). 4391 

 0.3512 

 0.3418 

 0.3295 



From this table is evident that in this summermonth by far the 

 highest temperatures are observed when there are calms ; for the 

 rest we have the lowest temperatures with the northerly seawind, 

 the highest with a landwind ; the transition from NNE (W 7°. 5 E 

 prop, dir.) to NE (N 30° E prop, dir.) is sharp, much sharper than 

 that from SW (N 210° E prop. dir. landwind) to WNW (N 277°.5 

 E proper dir. seawind). 



This sharp difference we do not find for the factor of consistency, 

 which shows tor WSW wind a distinct maximum and for calm a 

 minimum. 



the numbers of observations being rather slight for many directions 



