Art. l.-T. Tera.U: 



Tai-.lk I, 



The.se negative discrepancies are associated with the small values 

 of the daily temperature variation, as will be shown in subsequent 

 paragraplis. The abnormal values for Bozen and Klagenfurt are 

 evidently due to the altitude of the stations. 



In Northern America, negative J prevails in the inland, while 

 positive values are frequent in the coastal stations : 



Taiîi.i: II. 



