NO. 



EFFECT OF SOf.AR RADIATION CLAYTON 



II 



In this figure, A shows the mean of the correlations of temperature 

 for the tropical stations and subtropical land stations, B the mean of 

 the correlations of pressure for the tropical zone (inverted), C the 

 mean of the correlations of pressure for the temperate zone, D the 

 mean correlations of temperature for the temperate zone (inverted), 

 E the mean of the correlations of pressure for the Arctic circle 

 (inverted), and F the correlation of the temperature for Iceland. 



FIG. IV. 



Temperature in Tropics 

 Pressure in Tropics (^iaverted^ 



Pres ire in Ttmperate Zone 



Temperaiuic in Temperate Zone [[mveriedj 



Prejsurc In Arctic Circle QnvertedJ 

 Tempeiaturc in Iceland 



Fig. 4 



In each zone the pressure correlation was the reverse of that of 

 the temperature, when one was positive the other was negative. In 

 the plot the negative correlations were inverted or treated as positive 

 in order to show the progressive series of events from A to F . 



This plot indicates very clearly that in the tropical regions the 

 temperature rises and falls in unison with changes of solar radia- 

 tion, but follows the solar changes about two days. Following this 



