C 83 4 ) 
, After this manner I computed the following Table 
for every tenth Degree of Latitude, to the Equino&ial 
and Tropical Sun, by which an Eftimate may be made 
of the intermediate Degrees. 
Sun in 
Sua in 
Sim in 
Lit. 
S 
o 
20000 1 
18341 
J 1 
18341 
10 
19696 1 
20200 
s 
15824 
zo 
18794 1 
xi 737 
13166 
3° 
I732I 
22651 
IOI24 
i: , 4^ '_ 
1^321 
! *3°4 8 
6944 
So ' 
12855- 
22991 
379* 
6o 
I OOOO 
22773 
1075 
. 70 
684O 
000 
So 
3473 
24673 
000 
90 
. 0000 
25055 
000 
Thole that defire more of the Nature of this Pro- 
blem, as to the Geometry thereof, would do well to 
compare the XIII Prop. Cap. V. of the Learned Trea- 
tife, De Cdlculo Centri Gravitatis , by the Reverend 
Dr. Wa//is 9 Publiflied Anno. 1670. 
From this Rule there follow feveral Corollaries worth 
Note: As I. that the Equino&ialHeat when the Sun 
comes Vertical, is as twice the Square of Radius, which 
may be propofed as a Standard to compare with* in all 
other Cafes. II. That under the Equinoctial, the Heat 
is as the Sine of the Sun's Declination. III. That in the 
Frigid Zones when the Sun fets not, the Heat is as the 
Circumference of a Circle into the Sine of the Altitude 
%t 6. And confequently that in the fame Latitude thefe 
Aggregates of Warmth, are as the -Sines of the Suns 
Declinations ; and in the fame Declination of Sol, they 
are as the Sines of the Latitudes, and generally they are 
as the Si^w of the Latitudes into the Sines of Declina- 
tion. 
IV. That 
