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Earth, Sun, and Moon Interactions
Unit 1- Astronomy Earth, Sun, and Moon Interactions
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Rotation Spin/turn on an axis Earth’s tilt or axis is 23.5⁰ from the equator One rotation = one solar day (24 hrs/day) Foucault Pendulum- evidence of Earth’s rotation on its axis
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Revolution Move around an object; to orbit
A path the Earth follows around the sun Takes 1 year or days for Earth to travel around the Sun Causes seasons
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Solstice Summer Solstice- Winter Solstice-
Sun directly overhead at Tropic of Cancer 23.5 ⁰ north latitude June 21 each year Maximum daylight hours in northern hemisphere Winter Solstice- Sun directly overhead at Tropic of Capricorn 23.5 ⁰ south latitude December 21 each year Minimum daylight hours in northern hemisphere
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Equinox Vernal (Spring) and Autumnal (Fall) Equinox
“Equal night”- 12 hours of daylight, 12 hours of night Earth’s axis is NOT pointed at the Sun Both hemispheres receive equal amounts of sunlight
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Plane of Ecliptic = the plane in which Earth orbits around the Sun
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Stop to Summarize 1.) What’s the difference between rotation and revolution? 3.) How does the Earth’s tilt influence the equinoxes and solstices?
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Earth’s Shape OBLATE SHEROID
Equatorial Bulge- flattened sphere along the axis from pole to pole such that there is a bulge around the equator. - caused by the rotation of the Earth - the diameter at the equator is 43 km (kilometer) larger than the pole-to-pole diameter.
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Precession Precession
Slow and continuous change in the orientation of a Earth’s rotational axis Caused by the gravitational pull between the Sun and the Moon Changes the stars near the Pole Like a rotating toy top Occurs over a period 26,000 years
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