- The tidal force
is the stretching force
due to varying EXTERNAL
gravitational field.
The tidal force
is actually a combination of an ordinary
force
and an inertial forces
both of which originate with the EXTERNAL
gravitational field.
We will NOT go further into this somewhat complex topic.
- The tidal force
combined with the Earth's
self-gravity,
and pressure force,
and centrifugal force gives
the Earth its shape.
- Because the Moon is much closer
than the Sun,
it has a more rapidly varying
gravitational field
and that turns out to dominate over the overall stronger
gravitational field of the
Sun.
Hence the tidal force
of the Moon is stronger than that
of the Sun.
- When Moon
and Sun are aligned with
the Earth
(i.e., new moon or
full moon),
their tidal forces add and
tides are largest as aforesaid.
These tides are
spring tides
where "spring" has the meaning of the jump, burst forth, rise,
etc.
Coastal
storms that coincide with
spring tides
are particularly dangerous and prone to
cause flooding.
- When Moon
and Sun are at
a right angle
as seen from Earth
(i.e., first quarter moon
or
last quarter moon),
their tidal forces counteract each other, but
Moon's wins, but the
tides are smallest as aforesaid.
These tides are
neap tides.
"Neap is an Old English (AKA Anglo-Saxon)
word meaning without the power"
(Wikipedia:
Range variation: springs and neaps, slightly edited).
- Because of the
Earth's rotation
(counterclockwise
as seen from the north celestial pole (NCP))
relative to the
observable universe
(with period
sidereal day = 86164.0905 s = 0.997269566 days
= 1 day - 4 m + 4.0905 s (on average)),
the tide is continuously deforming
and reforming water bodies.
However, Moon also
orbits the Earth
(counterclockwise
as seen from the north celestial pole (NCP))
relative to the
observable universe
with
mean lunar sidereal month 27.321661547 days (J2000) ≅ 27.32166 days (to 7 digits) ≅ 27.3 days
Thus, the Moon's
rotation partially cancels the
Earth's rotation prolonging the
time between
high tides
to ∼ 12 hours and 25.2 minutes in most locations.
(Wikipedia:
Tide: Principal lunar semi-diurnal constituent).
So sailors have to have
tide tables handy so as to know
when the tides will be and how high/low they
will be.
For example, see Sven.
- As well as the water tide,
there is also an Earth tide---but we never
notice the continents
going up and down by a ∼ 1 meter about twice a day.
There's an atmospheric tide too
and furthermore:
- See Tide videos below
(local link /
general link: tide_videos.html).
EOF
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