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The Illusion of changing Lunar Size
Sequence of photos over Seattle, with the final one a longer exposure
Synodic vs Sidereal for the Moon
View of the Moon’s Orbit
Attributes of the Earth-Moon System
Making
Eclipses
Anatomy of Solar Eclipses
Eclipse
Tracks
Bailey’s Beads
Lunar Eclipses
A Lunar Eclipse
Share Question
In order for a solar eclipse to occur, the Moon must be:
a) high in the sky b) near first or last quarter c) near new moon d) near full moon e) over another country
Sequence of Lunar Phases
Orbital View of Lunar Phases
Geometry of Lunar Phases: Earth Perspective
Snapshots of Lunar Phases: What doesn’t
change?
Lunar Rotation
Share Question
As seen from the Moon, how often does the Sun rise? a) Never. b) About every 24 hours. c) About once per week. d) About once per month. e) About once per year.
As seen from the Moon, how often does the Earth set? a) Never. b) About every 24 hours. c) About once per week. d) About once per month. e) About once per year.
Prominent Lunar Missions
• Luna 3: 1959, Soviet1st pictures of Moon’s far side
• Apollo 11: July 20, 1969Astronauts Armstrong, Aldrin, and
Collins first on Moon• Apollos 11-17: 1969-1972
Returned ~400 kg of Lunar samples• Moon exploration continues to search for
water and to study its structure
Soviet Commemorative Stamps
Dark Side of the Moon
Apollo 11
Buzz Aldrin
Flag on the Moon
Lunar Footprint Mare Basalt
Highland Breccia Highland Anorthosite
Water Ice on the Moon
Lunar probes Clementine and Lunar Prospector have provided suggestive evidence for the existence of water ice in permanent shadows near the lunar poles.
Water Found on the Moon• Four spacecraft recently reported
small amounts of H2O and/or OH at the Moon:• India’s Chandrayaan mission•NASA’s Cassini mission•NASA’s EPOXI mission•NASA’s LCROSS mission
The first three measured the top few mm of the lunar surface. LCROSS measured plumes of lunar gas and soil ejected when a part of the spacecraft was crashed into a crater.
• How much water? Approximately 1 ton of lunar regolith will yield 1 liter of water
This false-color map created from data taken by NASA’s Moon Mineralogy Mapper (M3) on Chandrayaan is shaded blue where trace amounts of water (H2O) and hydroxyl (OH) lie in the top few mm of the surface.
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How was Water Detected?
• Lunar soil emits infrared thermal radiation. The amount of emitted light at each wavelength varies smoothly according to the Moon’s temperature.
• H2O or OH molecules in the soil absorb some of the radiation, but only at specific wavelengths
• All four infrared spectrographs measure absorption by water.
An infrared spectrum measured by LCROSS (black data points) compared to models (red line)
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Wavelengths where water absorbs light
model with thermal radiation only
model with thermal radiation and absorption by molecules
The Big Picture• Lunar water may come from ‘solar
wind’ hydrogen striking the surface, combining with oxygen in the soil. It may also arrive via meteorite and comet impacts. Both processes are likely.
• Lunar water may be ‘bounced’ by small impacts to polar regions, forming ice in permanently shadowed craters
• Similar processes may occur on other airless bodies (e.g., Mercury, asteroids)
• Water-laden lunar regolith may be a valuable resource, possibly supporting future lunar exploration activities
Discovery of water on the moon may support future activities on the lunar surface and beyond. Artwork from NASA / Pat Rawlings.
Tidal ForcesTidal forces are a consequence of how gravity from
one body acting on a second body varies across that second body.
Gravity isa) A vectorb) Changes with distance
Both Moon and Sun contribute to tides at the Earth (Sun’s tidal force about half of Moon’s)
Spring tide - when they add up (Sun, Earth, and Moon aligned at New and Full phases)
Neap tide - when tides are at odds (1st qtr. and 3rd qtr. Lunar phases)
The Tidal Force
Lunar Deformation
This is a false-color plot of the Moon’s deviation from spherical shape. Blue is “squashedness” (near the poles) and red is “stretchedness” (mostly at front and rear faces). Based on data from Clementine.
Roche LimitGravity scales like, FG ~ 1/r2
Tidal forces scale like, FT ~ 1/r3
Different dependence on distance suggests that tidal forces (although weak) could overcome surface gravity at some close distance, which is called the “Roche Limit”
One kind of Roche Limit is to ask how close a moon must come to a planet before the tidal force of the planet lifts a rock off the surface of the moon.
The Roche Limit
Tidal Evolution of Lunar Orbit
Lunar Surface
• Regolith – layer of rock and dust debris built up from meteoritic impacts
• Mare – few craters• Terrae – many craters• Galileo discovered Lunar craters in 1609• Craters:
– Reveals properties of sub-surface– Amount of cratering related to surface
age
Stretch of Lunar Terrain
Lunar “Climate”• The escape speed from the Moon is 2.3
km/sec, and so it has essentially no permanent atmosphere
• Moon does keep a transient atmosphere from capture of solar wind and radioactive decay in rocks (composition mainly He, Ne, Ar, and H)
• Without an atm., the sky is always “black”, and there are large day-night temperature swings, from 400 K (260 F) to 100 K (-280 F)– Earth has a 20 K (36 F) temperature swing on
average
Crater Formation
FEATURES:• Impact produces a crater• Sprays ejecta• Often leaves a rim• Sometimes with associated
bright rays (radial “spokes”, possibly a consequence of color contrast)
Crater Formation
Share Question
Why are some large crater walls sharp and steep, while others are more rounded?
a) different volcanos make different craters b) age differences c) size differences among the impact bodies d) composition differences among the impact
bodies e) seismic activity on the Moon
The Copernicus Crater
Rays
Crater Dating• Count number of craters, divide by
cratering rate, get an age!• CAUTIONS:
a) Erosionb) Cratering rate can vary over timec) Crater saturation – overcrowding (craters
upon craters)
• NOTE – Erosion can also bias relative numbers of different sized craters, since smaller craters tend to get “erased” faster.
Moon’s Interior
Origin of the Moon
1) [The Moon is old.]2) The chemical composition of the Moon
and Earth is similar but not identical.3) Near absence of the iron core in Moon.4) The Moon’s orbit is inclined to the Earth’s
equator, somewhat inclined to the ecliptic, and is prograde.
Models
• Fission Theory: Moon “spun off” from rapidly rotating Earth after iron core formed
• Binary Accretion Theory: formed as a pair
• Capture Theory: having formed elsewhere, the Moon was “captured” in a close encounter
• Giant Impact Theory: collision between Mars-sized body and Earth – debris collects to form our Moon
Model Schematics
Challenges
• Fission:– Moon’s orbit
inclined to Earth equator
– Needed rotation at once per 4 hrs – why was Earth so fast?
• Binary: – why no iron in
Moon?
• Capture:– Capture difficult
(how to slow down?)
– Are Earth and Moon compositions too similar?
• Giant Impact:– favored
Artistic Impression of Giant Impact
Giant Impact Theory
a. Similar composition to Earth because debris contains mantle material
b. Different composition owing to the impacting body
c. Moon’s orbit being inclined is not surprising
d. Body was iron-poor and Earth’s iron core was already formed