The Study of Astronomy, adapted to the capacities of youth: In twelve familiar dialogues, between a tutor and his pupil: explaining the general phænomena of the heavenly bodies, the theory of the tides, &c.Stedman, John, teacher of astronomy
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The Study of Astronomy, adapted to the capacities of youth: In twelve familiar dialogues, between a tutor and his pupil: explaining the general phænomena of the heavenly bodies, the theory of the tides, &c.
Stedman, John, teacher of astronomy
Astronomy -- Juvenile literature -- Early works to 1800
TUTOR. Most assuredly. For you see that the sun is over the tropic of
Capricorn, which you know is as much south of the equator as the tropic
of Cancer is north of it, where the sun was in our summer. The antarctic
circle is now enlightened, and the arctic obscured in shade; but, under
the equator there is neither increase nor decrease, the days and nights
being each twelve hours.
PUPIL. It is now our winter, the sun has been three months above the
horizon of the south pole, and will continue so till the vernal equinox,
when he will again rise to the north pole, and so on in regular
succession.
TUTOR. It must be plain then to you that there can be but one day and
one night at each of the poles, reckoning the time the sun is above or
below their respective horizons; under the arctic and antarctic circles,
the longest day is twenty-four hours, and in the shortest the sun is
just visible in the horizon at noon. The longest day decreases in length
the nearer we approach the equator, where I before observed there is no
variation, because the circle bounding light and darkness, in every
position of the earth, divides the equator into two equal parts; and, it
must be observed, that the longest day and longest night are equal to
each other in every part of the globe.
PUPIL. If the longest day under the arctic circle be just twenty-four
hours, the sun must rise in the north.
TUTOR. He does so, makes a complete circle and sets in the [15]north
again. From the arctic circle to the equator, he rises north of the east
and sets north of the west: at the equator he rises due east and sets
due west, thence southward to the antarctic circle, he rises south of
the east, and sets south of the west: and under the antarctic circle, as
I observed just now, he is visible in the horizon in the south at noon.
[Footnote 15: Here it must be observed that there will be a little
variation from sun-rising to sun-setting, as the earth is advancing
in its orbit.]
PUPIL. We usually say, the sun rises in the east and sets in the west.
TUTOR. At the equinoxes it must be so in all parts of the globe, the
poles excepted: in every other situation, except under the equator,
there is a continual change. What I have now told you, respecting the
northern hemisphere, will be reversed at our shortest day: that is, in
the northern hemisphere the sun will rise south of the east and set
south of the west; and, in the southern hemisphere the contrary, the sun
will be in the horizon, at noon, under the arctic circle, and the day
will be twenty-four hours under the antarctic circle.
PUPIL. Pray Sir, are the regions within the polar circles inhabited? If
they are, their situation, in winter, must, I think, be dreadful.
Public-domain text, read in full here on John Shaqi.
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