^^ • ■ Art. 6.— T. Terada : 



Type II. in which tlie years of minimum temperature are 



Fi ff. 12. Leh. 



Fio-. 13. 25 Continental station? 



.-associated with the small values of o, in analogy with Type II in 



the case of pressure. 



[ Type III. in which the area 



of the diagram njay conveniently 

 be divided into five sectors of 

 which the middle and the out- 

 ermost sectors contain the years 

 with maximum temperature, or in 

 other words, the maximum of 

 temperature occurs in the years 

 with small or large values of o and 

 the minimum occurs in those with 

 the intermediate values of this 

 solar quantity.'^ An example of 

 — this type is shown in Fig. 12. 

 Fig. 14. jacobshavn. Type IV. which is comple- 



1) The yearly fluctuations of mean temperature for 17 American, 7 European and. 1 

 Indian stations, given in p. 593 of Humphrey's " Physics of the Air", treated in the similar 

 manner, show a very typical diagram of this Type III (Fig. 13). Since these stations are all 

 ■continental, it may be said that this type is that characteristic for the land area. 



