178. The Atmosphere refracts the Sun’s rays so, as to bring him in sight every clear day, before he rises in the Horizon; and to keep him in view for some minutes after he is really set below it. For, at some times of the year, we see the Sun ten minutes longer above the Horizon than he would be if there were no refractions: and about six minutes every day at a mean rate.

Fig. IX.
[PLATE II].

179. To illustrate this, let IEK be a part of the Earth’s surface, covered with the Atmosphere HGFC; and let HEO be the[[43]] sensible Horizon of an observer at E. When the Sun is at A, really below the Horizon, a ray of light AC proceeding from him comes straight to C, where it falls on the surface of the Atmosphere, and there entering a denser medium, it is turned out of its rectilineal course ACdG, and bent down to the observer’s eye at E; who then sees the Sun in the direction of the refracted ray edE, which lies above the Horizon, and being extended out to the Heavens, shews the Sun at B § [171].

Fig. IX.

180. The higher the Sun rises, the less his rays are refracted, because they fall less obliquely on the surface of the Atmosphere § [172]. Thus, when the Sun is in the direction of the line EfL continued, he is so nearly perpendicular to the surface of the Earth at E, that his rays are but very little bent from a rectilineal course.

The quantity of refraction.

181. The Sun is about 3214 min. of a deg. in breadth, when at his mean distance from the Earth; and the horizontal refraction of his rays is 3334 min. which being more than his whole diameter, brings all his Disc in view, when his uppermost edge rises in the Horizon. At ten deg. height the refraction is not quite 5 min. at 20 deg. only 2 min. 26 sec.; at 30 deg. but 1 min. 32 sec.; between which and the Zenith, it is scarce sensible: the quantity throughout, is shewn by the annexed table, calculated by Sir Isaac Newton.

182. A Table shewing the Refractions of the Sun, Moon, and Stars; adapted to their apparent Altitudes.

Appar. Alt.Refraction. Ap. Alt.Refraction. Ap. Alt.Refraction.
D.M.M.S. D.M.S. D.M.S.
003345 21218 56036
0153024 22211 57035
0302735 2325 58034
0452511 24159 59032
10237 25154 60031
1152120 26149 61030
1301946 27144 62028
1451822 28140 63027
20178 29136 64026
230152 30132 65025
301320 31128 66024
3301157 32125 67023
401048 33122 68022
430950 34119 69021
5092 35116 70020
530821 36113 71019
60745 37111 72018
630714 3818 73017
70647 3916 74016
730622 4014 75015
8060 4112 76014
830540 4210 77013
90522 43058 78012
93056 44056 79011
100452 45054 80010
110427 46052 8109
12045 47050 8208
130347 48048 8307
140331 49047 8406
150317 50045 8505
16034 51044 8604
170253 52042 8703
180243 53040 8802
190234 54039 8911
200226 55038 9000

[PLATE II].
The inconstancy of Refractions.
A very remarkable case concerning refraction.