The description and use of the globes and the orrery: To which is prefix'd, by way of introduction, a brief account of the solar systemHarris, Joseph
History
The description and use of the globes and the orrery: To which is prefix'd, by way of introduction, a brief account of the solar system
Harris, Joseph
Astronomical models; Globes
Because the Sun, by his motion in the ecliptic, alters his declination
a small matter every day; if we suppose all the torrid zone to be
filled up with a spiral line, having so many turnings; or a screw
having so many threads, as the Sun is days in going from one tropic
to the other: And these threads at the same distance from one another
in all places, as the Sun alters his declination in one day in all
those places respectively: This spiral line or screw will represent
the apparent paths described by the Sun round the Earth every day; and
by following the thread from one tropic to the other, and back again,
we shall have the path the Sun seems to describe round the Earth in a
year. But because the inclinations of these threads to one another are
but small, we may suppose each diurnal path to be one of the parallels
of latitude, drawn, or supposed to be drawn upon the globe. Thus much
being premised, we shall explain this _Problem_, by placing the globe
according to some of the most remarkable positions of it, as before we
did for the most remarkable seasons of the year.
In the preceding problem, the globe being rectified according to the
Sun’s declination, the upper parts of the parallels of latitude,
represented the _Diurnal Arches_, or the length of the days all over
the world, at that particular time: Here we are to rectify the globe
according to the latitude of the place, and then the upper parts of the
parallels of declination are the diurnal arches; and the length of the
days at all times of the year, may be here determined by finding the
number of hours contained between the two extreme meridians, which cut
any parallel of declination in the Eastern and Western points of the
horizon; after the same manner, as before we found the length of the
day in the several latitudes at a particular time of the year.
1. Let the place proposed be under the equinoctial, and let the globe
be accordingly rectified for 00 degrees of latitude, which is called
a direct position of the sphere. Here all the parallels of latitude,
which in this case we will call the parallels of declination, are cut
by the horizon into two equal parts; and consequently those who live
under the equinoctial, have the days and nights of the same length at
all times of the year; and also in this part of the Earth, all the
_Stars_ rise and set, and their continuance above the horizon, is equal
to their stay below it, _viz._ 12 hours.
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