Astronomy Explained Upon Sir Isaac Newton's Principles: And made easy to those who have not studied mathematicsFerguson, James
Science
Astronomy Explained Upon Sir Isaac Newton's Principles: And made easy to those who have not studied mathematics
Ferguson, James
Astronomy -- Early works to 1800
304. When the Moon is in the Equator, the Tides are equally high in both
parts of the lunar day, or time of the Moon’s revolving from the
Meridian to the Meridian again, which is 24 hours 48 minutes. But as the
Moon declines from the Equator towards either Pole, the Tides are
alternately higher and lower at places having north or south Latitude.
For one of the highest elevations, which is that under the Moon, follows
her towards the same Pole, and the other declines towards the opposite;
each describing parallels as far distant from the Equator, on opposite
sides, as the Moon declines from it to either side; and consequently,
the parallels described by these elevations of the water are twice as
many degrees from one another, as the Moon is from the Equator;
increasing their distance as the Moon increases her declination, till it
be at the greatest, when the said parallels are, at a mean state, 47
degrees from one another: and on that day, the Tides are most unequal in
their heights. As the Moon returns toward the Equator, the parallels
described by the opposite elevations approach towards each other, until
the Moon comes to the Equator, and then they coincide. As the Moon
declines toward the opposite Pole, at equal distances, each elevation
describes the same parallel in the other part of the lunar day, which
it’s opposite elevation described before. Whilst the Moon has north
declination, the greatest Tides in the northern Hemisphere are when she
is above the Horizon; and the reverse whilst her declination is south.
Let _NESQ_ be the Earth, _NCS_ it’s Axis, _EQ_ the Equator, _T_♋ the
Tropic of Cancer, _t_♑ the Tropic of Capricorn, _ab_ the arctic Circle,
_cd_ the Antarctic, _N_ the north Pole, _S_ the south Pole, _M_ the
Moon, _F_ and _G_ the two eminences of water, whose lowest parts are at
_a_ and _d_ (Fig. III.) at _N_ and _S_ (Fig. IV.) and at _b_ and _c_
(Fig. V.) always 90 degrees from the highest. Now when the Moon is in
her greatest north declination at _M_, the highest elevation _G_ under
her, is on the Tropic of Cancer _T_♋, and the opposite elevation _F_ on
the Tropic of Capricorn _t_♑; and these two elevations describe the
Tropics by the Earth’s diurnal rotation. All places in the northern
Hemisphere _ENQ_ have the highest Tides when they come into the position
_b_♋_Q_, under the Moon; and the lowest Tides when the Earth’s diurnal
rotation carries them into the position _aTE_, on the side opposite to
the Moon; the reverse happens at the same time in the southern
Hemisphere _ESQ_, as is evident to sight. The Axis of the Tides _aCd_
has now it’s Poles _a_ and _d_ (being always 90 degrees from the highest
elevations) in the arctic and antarctic Circles; and therefore ’tis
plain, that at these Circles there is but one Tide of Flood, and one of
Ebb, in the lunar day. For, when the point _a_ revolves half round to
_b_, in 12 lunar hours, it has a Tide of Flood; but when it comes to the
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account