mercury

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Mercury

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Mercury. Mercury. Mercury. Mercury is always close to the sun!. What is being shown here?. The sun looks bigger from Mercury than from Earth. Effective Temperature : An estimate of the surface temperature of a planet, based only on its distance from the sun. Assumptions: - PowerPoint PPT Presentation

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Page 1: Mercury

Mercury

Page 2: Mercury
Page 3: Mercury
Page 4: Mercury
Page 5: Mercury
Page 6: Mercury

Mercury

Page 7: Mercury

Mercury

Page 8: Mercury

Mercury is always close to the sun!

Page 9: Mercury

What is being shown here?

Page 10: Mercury

The sun looks bigger from Mercury than from Earth

Page 11: Mercury

Effective Temperature : An estimate of the surface temperature of a

planet, based only on its distance from the sun

Assumptions:

Energy hitting surface of planet= Energy radiated by planet

Planet has no atmosphere

Planet absorbs all of the light that hits it

Page 12: Mercury

Effective Temperature : An estimate of the surface temperature of a

planet, based only on its distance from the sun

Planet Eff. Temp. Actual Surf Temps

Mercury 350° F -333-746° F

Venus 134° F 800-900° F

Earth 44° F 26-80° F

Mars -45° F -190- -10° F

Page 13: Mercury

What’s going on? Why is Mercury not uniformly hot?

Page 14: Mercury

Does Mercury have seasons like on Earth?

Page 15: Mercury

Winter on Earth Summer on Earth Any time on Earth!

Page 16: Mercury

One of these is a circle. One is Earth’s (elliptical) orbit.

Page 17: Mercury

Does Mercury have seasons like on Earth?

Page 18: Mercury

Does Mercury have seasons like on Earth?

Page 19: Mercury

Mercury’s orbital path around the sun

Mercury’s orbit has a higher eccentricity.Perihelion=closest approachAphelion=farthest distance

Page 20: Mercury

What is being shown here?

Page 21: Mercury

The Sun from Mercury at perihelion and aphelion

Page 22: Mercury

Orbital period:?

Rotation period: ?

Mercury has a 2:3 resonance between its spin and orbital periods. So every time Mercury goes ~2/3 of the way around the sun, it has rotated once.

For Earth:

Page 23: Mercury

Mercury has a 2:3 resonance between its spin and orbital periods. So every time Mercury goes ~2/3 of the way around the sun, it has rotated once.

Orbital period: 365 days

Rotation period: 1 day

For Earth:

Page 24: Mercury

Orbital period: 88 Earth days

Rotation period: 59 Earth days

Mercury has a 2:3 resonance between its spin and orbital periods. So every time Mercury goes ~2/3 of the way around the sun, it has rotated once.

Orbital period: 365 days

Rotation period: 1 day

For Earth: For Mercury:

Page 25: Mercury

Orbital period: 88 Earth days

Rotation period: 59 Earth days

Mercury has a 2:3 resonance between its spin and orbital periods. So every time Mercury goes ~2/3 of the way around the sun, it has rotated once.

Orbital period: 365 days

Rotation period: 1 day

For Earth: For Mercury:

Orbital period: 1 1/2 Mercury days

Rotation period: 1 Mercury day

Page 26: Mercury

Class Action: Terrestrial planets: Length of Mercury night

Page 27: Mercury

Messenger Animation: A day on Mercury

Page 28: Mercury

Also, the poles on Mercury never see sunlight!

Page 29: Mercury

Images of north polar region colored by amount of sunlight received

Page 30: Mercury

Summary of Mercury’s orbital characteristics:

-Mercury is much closer to the sun than Earth

-Mercury’s tilt is very low, so it does not have seasons caused by the tilt

-Its rotation period is almost equal to its orbital period, so there are long days, long nights

-Mercury’s orbit is eccentric so the sun changes size throughout the year

-Both the long days/long nights and eccentricity cause extreme temperature swings

-The poles of Mercury never see sunlight and can be very cold, so different parts of the surface of Mercury can be different temperatures

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Now let’s talk about Mercury’s interior and its geology

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Density is a measure of compactness.

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Density is a measure of compactness.

Page 34: Mercury

The density of rock is ~2.5 g/cm3. The density of iron is ~8 g/cm3. The density of terrestrial planets is ~5 g/cm3. Given this information, what are terrestrial planets most likely made of?

rock

Iron meteorite

(A) Rock

(B) Iron

(C) Both rock and iron

Page 35: Mercury

Mercury is small, and composed largely of iron.

Mercury

Earth

1800 km2400 km

Page 36: Mercury

How did Mercury get this dense?

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How did Mercury get this dense?Two ideas:

Heat from the early sun vaporized many of the rocky materials when Mercury was forming.

A giant impact stripped off the original crust and mantle.

Really, no one knows.

How might you test these hypotheses?

Page 38: Mercury

Does Mercury have an atmosphere?

Sort of. Hydrogen, Helium, Oxygen, Sodium, Potassium and Calcium have been detected.

But atmospheric pressures are very low

Why is this?

Page 39: Mercury

What is Mercury’s surface like?Mariner 10 (c. 1974) was the first and only spacecraft to visit Mercury before 2008.

Mariner 10 was a fly-by mission (it did not orbit the planet). Why do you think this is?

Page 40: Mercury

• Heavily cratered terrain

• Intercrater plains• The Caloris Basin• Antipodal terrain• Scarps

Mercury’s main geological features:

Page 41: Mercury
Page 42: Mercury

Heavily cratered highlands and intercrater plains

What caused the intercrater plains?

Page 43: Mercury

The Caloris Basin

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Caloris Antipode

Page 45: Mercury

Scarps and Ridges

These scarps are fault scarps.

What caused them?

Page 46: Mercury

Here is a fault scarp on the Earth (in Idaho)

http://skywalker.cochise.edu/wellerr/pglnx/chapter17x.htm

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Ice on Mercury??

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Messenger mission to Mercury.Launched in 2004.

Now orbiting Mercury!• Why is Mercury so dense?• What is the geologic history of

Mercury?• What is the structure of

Mercury's core?• What is the nature of Mercury's

magnetic field?• What are the unusual materials

at Mercury's poles?• What volatiles are important

at Mercury?

Page 49: Mercury

The Caloris Basin

Page 50: Mercury

The Caloris Basin

(a false color image)

Page 51: Mercury

The Caloris Antipode

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Strange “blue hollows” on Mercury represent never-before-seen minerals

Page 53: Mercury

Images of north polar region shows very reflective materials in shadowed regions (like craters)

Page 54: Mercury

Images of north polar region shows very reflective materials in shadowed regions (like craters)

Page 55: Mercury

The highest-resolution radar image of Mercury's south polar region made from the Arecibo Observatory (Harmon et al., Icarus, 211, 37-50, 2011) is shown in white on MESSENGER orbital images colorized by the faction of time the surface is illuminated. (Text: Marc Boucher)

Page 56: Mercury

Crater counting lecture tutorial

Page 57: Mercury

Why did Mercury end up in this state?

Planets like to be in ‘synchronous’ rotation because of tides. The closer a planet is to the sun, the stronger the tides.

in synchronous rotationdir. of orbital motion

rotating faster than synchronous

rotating slower than synchronous

dir. of orbital motion

dir. of orbital motion

Forces

Forces

Page 58: Mercury

Why did Mercury end up in this state?Mercury’s orbit is eccentric.

During which part of an orbit is the tidal force greatest? At this point of the orbit, does the planet move slower or faster than average?

To keep its bulges aligned while near this point, will it need to rotate faster or slower?

(For many years, scientists assumed Mercury was in synchronous rotation!)