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Year 1
Fundamentals of Ocean Physics
Tides
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7
% of the oceans surface is
continental shelf seas
gravity
natural phenomenon by which objects attract each other with a force proportional to their mass
strength of gravity is numerically equal to the
acceleration
of objects under its
influence
gravity=
9.81
m/s2
force fields is the
strength
of a
force
extended out into a plane that will weaken with
distance
Newtons First Law of Motion
a body continues in uniform
motion
in a
straight
line unless acted upon by
force
law of gravitational attraction
two
particle of
2
masses that are a
distance
apart are mutually attracted by a
force
equation for force
A)
G
B)
m1m2
C)
r
D)
2
4
as earth orbits sun, it
rotates
moon orbits earth in
27.3
days
lunar
phases
different angular position of the sun
the moon is at a
5
degree angle to the earth
moons gravitational force acts on
all
parts of earth
at any point, the
strength
of the moons gf is proportional to the
inverse
square of the
distance
from the earth
oceans will always
bulge
directly under the
moon
equilibrium tides
the earth experiencing two high and low tides a day
equilibrium
tides
1 bulge is from the
centrifugal force
, the other is from the
moon
on the other side of earth, the
centrifugal
force is will be
stronger
than the moons
gravitational
force
spring-neap tides
show the cycles of tides
spring tides happen after every
full
and
new
moon and earth,moon, and sun are
in
line
spring tides are
large
solar tide
a third smaller tide when the moon and suns gravityis opposing, reducing the hight of tide
Milanchovich
cycles
shape of earths orbit, angle of the earth, and the direction of the axis
tides are
semidiurnal
dominant tidal period is associated with the
moon
tidal
range
difference between the high and low water tidal levels
tidal
amplitude
half the tidal range
tidal
phase
time of high water relative to the HW time at Greenwich
tidal phase is measured at an
angle
long wave speed
A)
tidal amplitude
B)
V1
C)
(gD1)
D)
1/2
4
tidal speed
slows down
as the shelf depth
decreases
tidal waves get reflected by
coastlines
with
incoming
and
outcoming
waves
interacting
tidal resonance
tide excites one of the resonant modes of the ocean
tidal resonance map
of UK
time between tides averages at
12
hours and
25
minutes
speed of waves depend on the
depth
that they were travelling
wavelength is
long
compared to the
depth
of the ocean
waves travel at a speed equal to √(
gD
) where g is
gravity
and D is
water depth
tidal waves are directly produced by the
tide
generating
force
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