Tides Flashcards
For the tide analysis we distinguish two different theories:
- The theory of equilibrium after Newton
- The harmonic analysis after Laplace
The theory of equilibrium after Newton
The theory of equilibrium by Newton describes the tide as a result of the gravitational attraction between two ideal celestial bodies of masses m1 and m2 with the distance r to each other:
Force of attraction = Gm1m2/r^2
The attraction forces counteract centrifugal forces, as two celestial bodies are moving around a common center. The centrifugal forces on the celestial body of mass m1 and the distance e1 for common centroid can be calculated to:
Centrifugal Force = m1omega^2e1
The difference between attraction and local centrifugal force determines the tide generating force.
Harmonic Analysis after Laplace
Since the theory of equilibrium by Newton assumes an ideal celestial body with a constant water level above, the harmonic analysis of the tides after Laplace has been established, describing the tide as a summation of individual oscillation components of the amplitudes ai and phase Φi.
Which statements apply to the theory of equilibrium after Newton?
-A uniform water coverage of the earth is assumed.
-Dynamic effects and friction are not considered.
-The tide-generating forces are created due to the forces of the celestial bodies (forces of attraction and centrifugal forces)
How does the gravitational attraction between to masses relate to the distance between those two masses?
antiproportional to the square of the distance between the two masses
The centrifugal forces on the planets depend on
-the distance to the common center
-the rotational speed around the common center
-the mass of the celestial body
Astronomical frequencies and periods
solar day: 24h
lunar day: 1,03 MSD
tropical month: 27,32 MSD
tropical year: 365,24 MSD
julianic year: 8,85 years
nodaltide: 18,61 years
perihelion: 20900 years
MSD= mean solar day =24h
Full moon, new moon, half moon and their meaning for the different tides
Full moon: spring tide (superposition of lunar and solar tide)
new moon: spring tide (superposition of lunar and solar tide)
half moon: neap tide (lunar and solar tide partially cancel each other out)
Tidal Form Factor F
F=(K1+O1)/(M2+S2)
Form factor ranges and corresponding form names
F=0-0,25: semidiurnal form
F=0,25-1,50: mixed, predominantly semidiurnal form
F=1,50-3,00: mixed, predominantly diurnal form
F>3: diurnal form