Outlines of a mechanical theory of storms : $b containing the true law of lunar influence, with practical instructions to the navigator, to enable him approximately to calculate the coming changes of the wind and weather, for any given day, and for any part of the oceanBassnett, Thomas
Science
Outlines of a mechanical theory of storms : $b containing the true law of lunar influence, with practical instructions to the navigator, to enable him approximately to calculate the coming changes of the wind and weather, for any given day, and for any part of the ocean
Bassnett, Thomas
Weather
In the following figure, P is the pole of the earth; E the pole of the
ecliptic; L the pole of the lunar orbit; V the mean position of the pole
of the vortex at the time; the angle ♈EL the true longitude of the pole
of the lunar orbit, equal to the _true_ longitude of the ascending node
± 90°. VL is therefore the mean inclination ± 2° 45′; and the little
circle, the orbit described by the pole of the vortex _twice_ in each
sidereal revolution of the moon. The distance of the pole of the vortex
from the mean position V, may be approximately estimated, by multiplying
the maximum value 15′ by the sine of twice the moon's distance from the
node of the vortex, or from its mean position, viz.: the true longitude
of the ascending node of the moon on the ecliptic. From this we may
calculate the true place of the node, the true obliquity, and the true
inclination to the lunar orbit. Having indicated the necessity for this
correction, and its numerical coefficient, we shall no longer embarrass
the computation by such minutiæ, but consider the mean inclination as
the true inclination, and the mean place of the node as the true place
of the node, and coincident with the ascending node of the moon's orbit
on the ecliptic.
POSITION OF THE AXIS OF THE VORTEX.
It is now necessary to prove that the axis of the vortex will still pass
through the centre of gravity of the earth and moon.
[Illustration: Fig. 8]
Let XX now represent the axis of the lunar orbit, and C the centre of
gravity of the earth and moon, X′X′ the axis of the vortex, and KCR the
inclination of this axis. Then from
similarity Ct : Tt :: Cm : Mm
but Tt : Mm :: Moon's mass : Earth's mass.
That is Tt : Mm :: TC : MC.
Therefore the system is still balanced; and in no other point but the
point C, can the intersection of the axes be made without destroying
this balance.
It will be observed by inspecting the figure, that the arc R′K′ is
greater than the arc RK. That the first increases the arc AR, and the
second diminishes that arc. The arc R′K′ is a plus correction therefore,
and the smaller arc RK a minus correction. If the moon is between her
descending and ascending node, (taking now the node on the ecliptic,)
the correction is negative, and we take the smaller arc. If the moon is
between her ascending and descending node, the correction is positive,
and we take the larger arc. If the moon is 90° from the node, the
correction is a maximum. If the moon is at the node, the correction is
null. In all other positions it is as the sine of the moon's distance
from the nodes. We must now find the maximum value of these arcs of
correction corresponding to the mean inclination of 2° 45′.
To do this we may reduce TC to Tt in the ratio of radius to cosine of
the inclination, and taking TS for radius.
[Illustration: Fig. 9]
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