ARCTOWSKI, CHANGES IN DISTRIBUTION OF TEMPERATURE IQl 



■even sooner in Los Angeles, where it corresponds in time to the principal 

 antipleion of the curves of New York and Arequipa; but brax^hypleionian 

 particularities, such as the V-shaped depression of March, 1909,-Febru- 



FiG. 55. — Temperature variations in Montana, Nebraska, Kansas and Louisiana 



ary, 1910, appear later in Arequipa than in Eureka. The El Paso curve 

 •shows a variation opposite to that of Arequipa and retarded. The Corpus 

 Christi curve is more complicated, opposition and similarity of variation 

 being combined. ■ 



