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Earth’s MoonIt takes 27.3 days for the moon to
revolve around the Earth relative to a background star (sidereal month).
Because Earth also revolves around the Sun, it takes 2 more days for the moon to line up with the Earth and Sun again - (cycles of the moon, 29.5 days). Known as the synodic month.
How does the moon affect the Earth?
Tide: rise or fall in the ocean surfaceGravitational attraction between moon, sun, and
large bodies of waterThe closer the moon is to the water, the stronger
the pull; water on the side facing the moon is pulled more strongly toward the moon, producing a bulge and high tides.
https://www.youtube.com/watch?v=5ohDG7RqQ9I https://www.youtube.com/watch?v=IIMN-XVcpkE
How does the moon affect the Earth? Tide: rise or fall in the
ocean surface Gravitational
attraction between moon, sun, and large bodies of water
The closer the moon is to the water, the stronger the pull; water on the side facing the moon is pulled more strongly toward the moon, producing a bulge and high tides.
• https://www.youtube.com/watch?v=5ohDG7RqQ9I
• https://www.youtube.com/watch?v=IIMN-XVcpkE
Problem: Moon rises an average of 52.7 minutes later each day. You can use this formula:
TN = To + N x 52.7 minutes
Where TN = the time of high tide in 7 days
To = the original time of high tide
N = number of days later for which you want to determine the high tide
If the original high tide is 1:00 pm, find the time of high tide in 7 days.
TN = 1:00 pm + 7 x 52.7 min
= 1:00 pm + 369 min
= 1:00 pm + 6 hr 09 min
= 7:09 pm
Moonlight
The Moon shines because it reflects sunlight from its surface
As Moon orbits the Earth, different areas of the side that faces earth reflects sunlight, causing Moon’s appearance to change
Phases of the MoonNew Moon – Occurs when the Moon is between the
Earth and SunAfter new moon, moon phases are waxing (Moon
appears to grow larger)Waxing crescent - The first phase after new moonFirst quarter Moon - About a week after new moon;
half of Moon is visibleWaxing gibbous – from first quarter Moon until full
MoonFull moon – when side of the Moon facing us is
entirely illuminated, Earth is between Moon and Sun
Phases of the Moon
After full moon, moon phases are waning (Moon appears to grow smaller)Waning gibbous crescent – from full moon to 3rd
quarter Moon3rd quarter Moon -half of Moon is visibleWaning crescent –small sliver New moon
If 2 full moons in one month (29.5 days/one lunar cycle), then second full moon is sometimes called a blue moon
Solar Eclipse• When the moon moves directly between Sun
and Earth and casts shadow on the Earth.• Umbra - Darkest portion of the moon’s shadow• Penumbra – lighter shadow on Earth’s surface
that surrounds the umbra
Videos
https://www.youtube.com/watch?v=NCweccNOaqo
https://www.youtube.com/watch?v=xBc8QHSsFgE
Lunar eclipseWhen the Earth passes between the Sun
and the Moon and casts a shadow on the Moon
Begins when Moon moves into Earth’s penumbra, moving into Earth’s umbra
Can only occur when Moon enters a full moon phase
Partial lunar eclipse: occurs when a portion of the Moon moves into earth’s umbra; the remaining portion of the Moon is in earth’s penumbra and receives some direct sunlight
Frequency of Eclipse
Total solar eclipse: Up to twice/year, but most people don’t see itOnly those people living in small area where
moon’s umbra strikes Earth can see total solar eclipse
Total lunar eclipse – more frequently observed because all of the Moon is in Earth’s umbra,
so anyone on the night side of Earth could see it
Moon’s Surface
• Craters: depressions on the moon’s surface created by impacts from asteroids and comets
• Mountains (highlands): areas that were thrust upward from the impact events
Moon’s Surface
o Maria: surface features which are dark colored, flat, lava filled regions Created when cracks
formed in the crust from the impact of asteroids/comets, the cracks allowed lava to flow into craters and fill them
Moon’s Surface
o Regolith: layer of dusty lunar material produced by collisions between asteroids and comets and the Moon; can be up to 40 m thick
Moon’s Interioro Seismographs left on moon’s surface revealed
Crust
Mantle
Core
o Maria on Moon’s surface suggests the interior of the moon must have been molten at one time
Origin of Moon
Giant Impact Theory:
o Moon formed about 4.4 billion year ago when Mars-sized object collided with Earth
o The cores of the 2 bodies combined and settled toward the center of primitive Earth
o Some gas and rock thrown into orbit; remainder condensed into mass which formed moon
o Explains why Earth and Moon similar, but not identical
Earth
Evidence for Earth’s shape as a sphereo No matter where you
are on earth, objects fall straight down (gravity)
o Earth’s shadow on the Moon during a lunar eclipse is always curved
o People in different parts of the world see different stars at night
Earth’s shape
o Gravity is responsible for Earth's shape
o Astronomers think Earth formed as objects in solar system crashed into each other and combined because of gravitational attraction
o Energy released as objects crashed into growing Earth to be molten
o Gravity caused molten Earth to form sphere
o As Earth cooled over time, different layers formed due to differences in density, becoming the inner core, outer core, mantle and crust
Earth’s Magnetic Fieldo Magnetic field: Scientists hypothesize it is the
result of Earth’s rotation and the circulation of molten metals in outer core
o Magnetic reversals: location of magnetic poles change over time; large-scale magnetic reversals occur on average every 200,000 years
o Auroras: Sun produces solar winds (streams of electrically charged particles). The magnetosphere deflects these harmful particles, causing them to spiral along Earth’s magnetic field. They eventually collide with atoms and molecules in Earth’s atmosphere, causing them to emit light.
Planet Eartho The orbit of Earth
around the Sun is elliptical.
o An ellipse is an elongated closed curve with two foci.
o The distance of the Earth to the Sun varies
o The Earth is closest to the Sun in January (147 million km) and is farthest away in early July (152 million km)
Earth in the Solar System
Venuso Venus nearly same size
of Earth
o Atmosphere contains 96% CO2 (carbon dioxide) – Earth contains 0.04%. Earth’s oceans absorbed much of it
o High CO2 creates greenhouse effect – temperatures of +460°C (Earth average is 15°C).
Marso Slightly half the
diameter of Earth; gravitational pull only 38% as strong, not strong enough to hold dense atmosphere so average surface temperature is -63°C
o Mars lacks magnetic field, which allows atmosphere to be stripped away by solar wind