General Astronomy
description
Transcript of General Astronomy
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General Astronomy
Earth and Moon
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The Double PlanetThe Earth-Moon system is unique in this solar system in that
Earth's moon is the largest in relation to its planet.
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Earth, Terra, Sol III What's in a name?
Apollo 17
This is where you live.
This is where all of your ancestors have ever lived.
Yours may be the first generation who's children may live elsewhere.
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The Moon, Luna, Selene
Taylor Observatory Stockton 5" Celestron
This is where some may live in the future
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Physical ParametersBefore comparing the planets, let's look as some of the physical
characteristics:Density – Mass divided by volume
This gives us an idea of the composition of the body. If we can measure the radius and (from Kepler's 3rd Law) the mass, then we can get the density.
Some densities: (in grams/cubic centimeter)
Pure Water 1.0
Ice 0.917Most Minerals 2.5 – 4.0Iron 7.9
Of course, a planet is a mixture – so the actual density depends on how much of each type of item is present.
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Obliquity – The 'tilt' of the north-south (rotational) axis with respect to the Ecliptic.
Earth's inclination is 23.5 degrees
Physical Parameters
Inclination – The 'tilt' of the orbit with respect to the Ecliptic
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Oblateness - The flattening at the polesPhysical Parameters
Albedo - The amount of light reflected from the surface expressed as a fraction; eg, 100% reflection = 1.0
0.0 .40 .60 1.0
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Earth
Physical Characterstics
Radius 6,371 KmDensity 5.52 g/ccRotation 23h56m04s
Inclination 0ºObliquity 23º 27'Oblateness 1/298.2Albedo 0.39Escape Vel. 11.2 Km/s
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The Moon
Physical Characteristics
Radius 1,738 KmDensity 3.34 g/ccAlbedo 0.12Escape Vel. 1.9 Km/s
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Lunar Features
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The Far SideIt's easy to see that the far side of the Moon is much rougher.There are many more impact craters and much fewer marias.
This makes sense when you realize the Earth has been 'protecting' the near side
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Ice on the Moon?• A recent mission called Lunar Prospector has
reported possible evidence for ice on the Moon:• The Moon has permanently shadowed polar
craters too.• Data showed slightly enhanced Hydrogen in these
areas.• Not confirmed by radar images as on Mercury.• H could be from solar wind or some other process
and• might not be the "H" in H2O.• Big implications for space exploration.
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Lunar Water – Sept 2009NASA's Moon Mineralogy Mapper, an instrument on the Indian Space Research Organization's Chandrayaan-1 mission, took this image of Earth's moon.
It is a three-color composite of reflected near-infrared radiation from the sun, and illustrates the extent to which different materials are mapped across the side of the moon that faces Earth.
Small amounts of water were detected on the surface of the moon at various locations. This image illustrates their distribution at high latitudes toward the poles.
Blue shows the signature of water, green shows the brightness of the surface as measured by reflected infrared radiation from the sun and red shows an iron-bearing mineral called pyroxene.
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Lunar Water – Sept 2009
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Lunar Water – Sept 2009
On the left is an image showing brightness at shorter infrared wavelengths. On the right, the distribution of water-rich minerals (light blue) is shown around a small crater. Both water- and hydroxyl-rich (red) materials were found to be associated with material ejected from the crater.
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Lunar Cratering
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Ages of SurfacesDating of Moon rocks allow us to measure when the rock was last melted…
…when were most craters made?
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What is the order from oldest to youngest?
A (volcano)
B (crater)
C (crater)D (lava flow from another volcano)
A, C, D, B
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Buzz Aldrin (photo by Neil Armstrong)
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RetroreflectorLeft on the lunar surface by the Apollo astronauts, this instrument is used to reflect laser beams back to Earth and accurately measure the moon's distance.Hard to do if the Moon landings were a hoax.
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• A blue moon is when more than one full moon occurs in the same calendar month. The 2nd occurance is the blue moon• The moon undergoes synchronous rotation and revolution (i.e. the periods of rotation and revolution are identical), so one side of the moon always faces the Earth.
• The harvest moon involves the rising of the full moon in late September and early October.
Moon Factoids
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• The phase of the moon has no effect on human behavior.
• There is no such thing as the “darkside of the moon.”
• We did indeed land humans on the moon in the six Apollo landings between July 1969 and December 1972.
Moon Myths
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Mythbusters!
There is no relationship between the full moon and the number of births
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Earth-Moon InteractionsObvious interactions we must examine
are:
1. Phases of the Moon (Reprise)2. Eclipses3. Tides
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N.P. Noon
Sunset
Midnight
Sunrise
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New
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Sunset
New
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Waxing Crescent
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Sunset
Waxing Crescent
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First Quarter
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Sunset
First Quarter
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Waxing Gibbous
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Sunset
Waxing Gibbous
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Full
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Sunset
Full
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Sunrise
Full
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Waning Gibbous
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Sunrise
Waning Gibbous
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Last Quarter
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Sunrise
Last Quarter
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Waning Crescent
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Sunrise
Waning Crescent
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New
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Sunrise
New
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The Phases
about 1 week for each quarter (like newfirst quarter)
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New Waxing Crescent
First Quarter
Waxing Gibbous
Full Waning Gibbous
Last Quarter
Waning Crescent
New
Lunar Phases
Lunar or Synodic Month: 29 1/2 days
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Sidereal and Synodic Months
SUN
• synodic month: time for Moon to make one circle of sky compared to Sun
• sidereal month: time for Moon to make one circle of sky compared to stars
SUN
27.3 d 29.5 d
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The Earth's ShadowThe Earth will cast two shadows. One where all the light is blocked and a second where only part of the light is blocked
The darker, innermost shadow is the Umbra
The lighter, surrounding shadow is the Penumbra
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Shadows
total shadow: UMBRApartial shadow: PENUMBRA
lower edge of Sun blocked from view
upper edge of Sun blocked from view
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Lunar Eclipse
Moon
When the Moon enters the Earth's shadow, we have a lunar eclipse
This, of course, can only occur at the time of the Full Moon
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Lunar Eclipse
A total eclipse of the moon.
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Solar EclipseAt the time of the New Moon, the Moon casts its shadow(s) on the Earth
The Moon's shadows are much smaller and only cover a small area on the Earth. If you are in the penumbra, you see a Partial EclipseIf you are in the umbra, you see a Total Eclipse
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EclipsesSo if a Lunar eclipse occurs at a full
moon and a Solar eclipse occurs at a new moon, why don't we see each type of eclipse every month?
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Inclination of Orbits
The moon's orbit is a bit over 5° inclinationThis means that most times it misses theEarth's shadow – too high or too low
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Eclipses
Earth and lunar shadows, shown at proper scale, illustrate why eclipses occur infrequently.
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Path of Totality - 2017
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Total Eclipse - 2017Pomona, NJPartial Eclipse
Salem, ORTotal Eclipse
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Total Eclipse - 2017Salem, OR
Start of eclipse
Ha
TotalityCrescents through the leaves
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Bailey’s Beads
Solar Corona
“Diamond Ring”
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The orbits of the moon and Earth are elliptical, which affects the angular diameters of the moon and sun.
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An annular eclipse
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Lunar Shadow from Mir
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Lunar Shadow passing over Africa
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The tides are caused by the differential forces of the moon's gravitational pull. The term differential forces implies the differences at varying points on the Earth - it should be clear since gravitational force depend on distance that the force on the point directly beneath the moon will be greater than at any other point. As the Lunar gravity pulls on the water, it flows to that spot as best it can.
The Tides
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Tides
Ignoring the actual geography and shape of the Earth this leads to a simple (and incorrect) model of the tides
Why is this incorrect?To see, let's ignore the orbital motions and look at the daily rotation of the Earth
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X Noon: High Tide
X
6PM MidTide
X
6AM MidTide
XMidnight: Low Tide
One High tide per day? That can't be right!
Noon 6AM Midnight 6AM
Tides
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XNoon: High Tide
X
6PM LowTide
X
6AM LowTide
XMidnight: High Tide
Noon 6PM Midnight 6AM
Tides
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• Of course the Tides are more complicated than this simple picture.– The moon also moves in its orbit– Geography becomes a significant
factor– The moon and the earth are inclined
to the ecliptic– The Sun's gravitational pull creates
tides of about 50% of those caused by the Moon
Tides
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Adding the Sun's Effects
When the sun and moon are lined up, during a full moon and a new moon, the tides caused by each augment each other giving higher highs and lower lows.
These are known as
Spring Tides
When the moon's direction is at right angles to the sun, the tides tend to cancel each other leading to lower highs and higher lows.
These are known asNeap Tides
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TidesNow let's see what 'geography' can do to
the tides.For example, the Delaware River is a tidal
estuary. It takes the tide about six hours to move from the mouth of the Delaware Bay to Philadelphia. So when it's high tide at Cape May, it is low tide at Philly and vice versa.
A more impressive effect, however, is farther north…
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Bay of Fundy, NS, CanadaAt low tide, the Bay is an interesting place to walk and explore. Ocean bottom as far as the eye can see…
But, don't wander too far from shore. The tide can rise nearly 17 meters
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Tidal Friction• As the oceans are constantly being
pulled about the Earth by Lunar and Solar gravity, there is friction. Where there is friction, there is energy loss resulting in a slowing down of the Earth's rotational speed.
• The days are getting longer increasing by several milliseconds each century
• Since the earth and moon form a system this slowing also affects the moon. The moon is slowly receeding from the earth.
• Eventually, the Earth and Moon will always keep the same face to each other
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Magnetic Field EffectsThe Earth's magnetic field is also very
important to those who live on its surface.– The obvious uses for navigation – both for
humans and migrating birds– More importantly, the magnetic field protects
us from the Sun• The Sun is constantly emitting streams of charged
particles (as well as light and warmth)• If all of these were to hit the surface, life would
likely not exist.– The magnetic field forms a protective barrier
trapping much of the oncoming particles and channeling some of the more intense into the north and south poles.
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The Magnetosphere
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Magnetic Field Effects• As the charged particles (protons, electron and other
ions) follow the magnetic field lines into the poles, they strike atoms in the atmosphere causing them to emit light. This light is known as the aurora– Aurora borealis (Northern Lights)– Aurora austrialis (Southern Lights)
Photos by Jan Curtis, Fairbanks, AK
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Northern Lights From Above and Below
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Van Allen Radiation BeltsThese are two torus
shaped areas of intense radiation where energetic particles from the sun are trapped by the earth's magnetic field.
The inner belt is about 4,000 miles out, and the outer about 10,000 miles
Note how the sunward side is compressed by the Solar Wind.
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The Ozone HoleOzone (O3) absorbs in the ultraviolet and protects us, animals and plants.Clorofluorocarbons (freons) and halons (bromine) when they get into the upper regions of the atmosphere break down and the chlorine and bromine work to reduce the available ozone.
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The Earth’s InteriorSeismology- Study of how earthquake vibrations propagate through the Earth’sinterior.
Material of the Earth reflects and bends seismic waves:p – primary waves (longitudinal waves) Propagate through solids and liquids.s – secondary waves (transverse waves) Propagate through only through solids.
Solid inner core, liquid outer core, mantle, crust
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Shaping the EarthFormation of topographic
relief– Volcanism– Tectonism– Impacts
Leveling of the Earth’s surface– Gradation
Continental Drift
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The Earth at Night