310 Prof. Baifour Stewart and Mr. W. L. Carpenter. 



terrestrial Inequalities as in the previous instance. The series of 

 years is the same, and the same use is made of the Kew temperature- 

 ranges as in the Inequalities around 24 days. 



In the Table V (p. 309) we have, inclosed in brackets, the positions 

 of all sufficiently well-defined maximum Inequalities, whether of sun- 

 spots or Toronto temperature-ranges. It will be seen, as in the 

 previous case, that the positions of maximum apparent Inequalities 

 for sun-spots are near those for Toronto temperature-ranges ; and the 

 same remarks are here applicable which have already been made. 



20. Constancy of Type in the various Inequalities. Here, as in the 

 Inequalities around 24 days, the Toronto temperature-ranges present 

 on the whole two maxima and two minima, the sun-spots one well- 

 defined maximum and minimum ; and the Kew temperature-ranges 

 one maximum and minimum, not so well defined. 



21. Comparison in Phase. For the purpose of making this com- 

 parison, we proceed to discuss the various couplets of Table V, taking 

 as before the' time-scales in our comparison from the Toronto tem- 

 perature Inequalities rather than from the sun-spots.* 



SS-.J8, TT_ 52 . Toronto temperature-range Inequality not sufficiently 

 near the type ; the others good. 



* It will be desirable to exhibit the rejected Inequalities. They are as follows, 

 being the aggregate for 36 years in TT, and for 24 years in KT : 



