478 



H. MOHN. METEOEOLOGY. 



[NORW. POL. EXP. 



In order to study the relation between the diurnal period of the tempera- 

 ture of the air and the velocity of the wind, I have made computations similar 

 to those worked out above (p. 299 to 303), and give the results in the 

 following Tables. 



