ARCTOWSKI, CHANGES IN DISTRIBUTION OF TEMPERATURE 105 



sions, that it is perfectly safe to say that the records of Greenland and 

 Iceland are entirely sufficient for the purpose of the questions I had to 

 solve. 



In Table VI, I give the annual departures from the ten-yearly means 

 of temperature for the stations now taken into consideration, the dia- 



FiG. 57. — Temperature variations in Greenland, IceJand and Faroe 



grams (Figs. 57-60) express graphically the succession of consecutive 

 means, and in Table VII, I give the highest and lowest of these values 

 as well as their differences. 



