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Motions of the Earth-Moon System
• Orbital period = about one month
• The moon’s orbit is elliptical
• It is tilted 5 degrees off of Earth’s orbital plane
Perigee: Moon is closest to Earth Apogee: Moon is farthest from Earth
Average distance from Earth to the moon = 384,000 km = 238,607 miles!
Phases of the Moon
• phases: various shapes of the moon lighted by reflected sunlight
Brain Pop:
Moon Phases
• waxing: when the size of the visible portion of the moon is increasing
• waning: when the size of the visible portion of the moon is decreasing
• new moon: no lighted area of the moon is visible from the Earth
•full moon: entire half of the side of the moon facing Earth is lit
• crescent: less than half of the side facing the Earth is lit
•gibbous: more than half of the side facing the Earth is lit
Lunar Motions • Synodic Month: The cycling of the moon through its phases (Apparent Motion)
• 29 1/2 days • Basis for the first Roman calendar
• Siderial Month: The moon revolutionary period around the earth (Actual Motion)
• 27 1/3 days
•Occurs because Earth is revolving around the sun at the same time as the moon is revolving around The Earth!
• Why does the same side of the moon always face us?
• Because the moon rotates and revolves at the same speed:
27 1/3 days!
Eclipses
• when one planetary body passes through the shadow of another
Brain Pop:
Eclipse
• Eclipses don’t occur every month because the moons orbit is tilted with respect to the Earth’s orbit
Tides Daily changes in the elevation of the ocean surface
Result from gravitational attraction between… Earth, Moon, & Sun
Brain Pop:
Tides
The earth has a uniform level of water all around it.
2 forces act on the water to produce tides…
The moon’s GRAVITY pulls on the earth, and the water bulges toward the moon.
Because the earth is spinning, there is a force pulling water in the opposite direction INERTIA
As the earth turns upon its own axis in about 24 hours, a point on the earth moves through areas with these different forces acting on it.
The Result…
Neap Tide – daily tidal
range is lower than average because the
gravity of the sun & moon counteract each other
Tidal Patterns
Diurnal - One high tide & one low tide each day
Semidiurnal - Two high tides & Two low tides each day