174 
FIFTH REPORT— 1335 . 
Table of the Differences between the Ratios of the Quantities 
of Rain at the Upper, Middle , and Lower Stations , in rela¬ 
tion to the Temperature of the Season. 
Temp. 
Differences from 
100. 
Sum of 
d + d’. 
4 
t' 
d 
d' 
3 summer months.... 
o 
608 
33-65 
14-17 
47-82 
48-12 
5 warmer months .... 
58*5 
35-18 
15-50 
5068 
50 00 
7 warmer months.... 
551 
35-58 
1616 
51-74 
52-93 
7 colder months. 
40-8 
46-42 
26-18 
72-60 
70-10 
5 colder months...... 
39-3 
47-40 
26-38 
73-78 
74-47 
3 winter months .... 
36-3 
50*06 
29-74 
79-80 
80-61 
Whole year . 
. 48-2 (— t ) 
60-71 
A 
60-71 
The last column gives the numbers corresponding to the 
simple formula A which shows clearly the real dependence 
of the amount of the diminution of rain at the upper stations 
upon the temperature of the season inversely. 
The dependence of the ratio of the differences of rain, at 
diffferent elevations above the ground, upon the height of the 
stations, will appear from the following tables : 
Table to show the Mean Annual Value, of the Function of the 
Height (<p h). 
Quantities. 
Differences from 
100. 
Resulting 
value 
d. 
d'. 
of <p h. 
Inches. 
Inches. 
Inches. 
First series .. 
15-715 
20-182 
23-785 
33-90 
14-70 
h‘53 
h'3S 
Second do. 
14-963 
19-850 
25-706 
41-79 
22-78 
Third do. 
8-294 
12-135 
15-939 
47-97 
23-87 
ll^ 
General mean of) 
three years .. .. j 
12*990 
17-389 
21-810 
40-44 
20-27 
k-437 
Mean of the differences from 100 . 
41-22 
20-45 
/,-443 
