CLIMATOLOGICAL AVERAGES — -VON BEZOLD 



425 



If we compare this result of the formula, not as above with the 

 holospheric value t= %(t +(p + /_^), but directly with the numbers 

 given by Spitaler and Batch elder for the individual latitude circles, 

 then the departures between computation and observation are of 

 course somewhat larger but still they are always within moderate 

 limits. 



We see this from the accompanying table iv, which also provides 

 an interesting survey of the different relations of the two hemi- 

 spheres. 



Table IV. Comparison between the hemispheric values deduced from observa- 

 tions and the computed values 



If now we use the sine as the argument we obtain the following 

 tables v and vi. 



Table V. Comparison between the holospheric 'values deduced from observa- 

 tions and the computed values 



