the other terrestrial planets · atmosphere, forming a bow shock and a long ion tail. co 2 produced...
TRANSCRIPT
The Other Terrestrial Planets
Mercury
View from Earth
Doppler Effect
Rotation and
Revolution
Surface Features
History
Earth Mercury
Semi-major Axis 1 A.U. 0.387 A.U.
Inclination 0° 7°
Orbital period 1.000 tropical year 87.97 days
Orbital eccentricity 0.017 0.206
Rotational period 23 h 56 min 4.1 s 58.65 days
Tilt 23° 27’ 0°
Radius 6378 km 2439 km
Mass 5.97 x1024 kg 3.30 x 1023 kg
Bulk density 5.52 g/cm3 5.43 g/cm3
Atmosphere N2, O2 trace Na, K, H2, He
Albedo 0.40 0.06
Surface temperature 250-300 K 100-700 K
Escape speed 11.2 km/s 4.3 km/s
Magnetic moment (equator) 8 x 1010 G.km3 4.8 x 107 G.km3
Phases of Mercury can be seen best when
Mercury is at its maximum elongation
Viewing Mercury from Earth
Measuring Mercury’s Rotation:
the Doppler Effect
Blue Shift (to higher
frequencies) Red Shift (to lower
frequencies)
The light of a moving
source is blue/red
shifted by
Dl/l0 = vr/c
l0 = actual
wavelength emitted
by the source
Dl = l - l0
wavelength change
from the Doppler
effect
vr = radial velocity
vr
Example 1 of the Doppler Effect Earth’s orbital motion around the Sun causes a
radial velocity towards (or away from) any star.
Example 2 of the Doppler Effect Take λ0 of the Hα (Balmer alpha) line:
λ0 = 656 nm
Assume, we observe a star’s spectrum with the Hα line at λ = 658 nm. Then,
Δ λ = 2 nm.
We find Δλ / λ0 = 0.003 = 3 x 10-3
Thus,
vr/c = 0.003,
or
vr = c Δλ / λ0 = 300,000 km/s x 0.003 = 900 km/s
Because the value is positive, the line is red shifted, so the star is receding from us with a radial velocity
of 900 km/s.
Doppler
Effect:
Planetary
Rotation Radar is bounced
off the two sides of
the planet. The
Doppler shift is
used to determine
the rotation velocity.
With the
measurement of the
circumference of the
planet, the rotation
period can be
calculated.
Rotation and Revolution of Mercury Like Earth’s Moon (tidally locked to revolution around Earth),
Mercury’s rotation has been altered by the Sun’s tidal forces,
but it has not locked into a 1:1 spin-orbit resonance. It is in a
3:2 resonance. Revolution period = 3/2 times rotation period.
Revolution: ≈ 88 days, Rotation: ≈ 59 days
Extreme day-night temperature contrast: 100 K (-173 oC) – 600 K (330 oC)
Spacecraft Exploration of Mercury
Mariner 10: flew by
Mercury, 1974–75
Spacecraft Exploration of Mercury
The Messenger
spacecraft was
launched in
August 2004. It
flew by Mercury
in January and
October, 2008
and September,
2009. It was put
in orbit around
Mercury in
March, 2011.
Mercury is very similar to the Moon in several ways:
• Small; no atmosphere
• Lowlands flooded by ancient lava flows
• Heavily cratered surfaces
Mercury
Lobate Scarps
Curved cliffs, several hundred km long and up to 3
km high, probably formed when Mercury shrunk
while cooling down
Mariner 10
Messenger
The Caloris
Basin, is a very
large impact
feature that is
not as
completely
flooded as the
mare of the
Moon
Caloris Basin
The Surface of Mercury Weird terrain was found on the opposite side of the planet from the
Caloris Basin . Weird terrain was subsequently found on the far
side of the Moon opposite large basins.
History of Mercury
1) Formed about 4.6 million years ago
2) It melted from impact energy and cooled
slowly
3) Differentiation to form metallic core and
rocky mantle
4) Major impact might have melted and
ejected much of the mantle
5) Interior shrank, crumpling the solid crust
6) Massive meteorite bombardment
Cratering; lava flows
Venus
Rotation
Atmosphere
Surface Features
History
Earth Venus
Semi-major Axis 1 A.U. 0.723 A.U.
Inclination 0° 3° 23’
Orbital period 1.000 tropical year 224.7 days
Orbital eccentricity 0.017 0.007
Rotational period 23 h 56 min 4.1 s 243.01 days—retro
Tilt 23° 27’ 117° 18’
Radius 6378 km 6052 km
Mass 5.97 x1024 kg 4.87 x 1024 kg
Bulk density 5.52 g/cm3 5.24 g/cm3
Atmosphere N2, O2 CO2, N2
Albedo 0.40 0.76
Surface temperature 250-300 K 700 K
Escape speed 11.2 km/s 10.4 km/s
Magnetic moment (equator) 8 x 1010 G.km3 >4 x 106 G.km3
The Rotation of Venus
Almost all planets rotate
counterclockwise (prograde
rotation), i.e. in the same sense as
orbital motion.
Exceptions: Venus, Uranus and
Pluto
Venus rotates clockwise
(retrograde rotation), with a period
slightly longer than the orbital
period.
Possible reasons:
Tidal forces of the Sun on a
molten core
Off-center collision with a
massive protoplanet
Long-Distance Observations of Venus
Dense atmosphere and
thick clouds make the
surface impossible to
see
The surface temperature
is about 730 K – hotter
than Mercury!
Spacecraft Exploration of Venus Soviet Venera probes landed on Venus from
1970–1978
The Magellan spacecraft mapped Venus using
synthetic aperture radar from 1990-1994
The Atmosphere of Venus
Venus’s atmosphere
is very dense (~100 x
pressure of Earth’s)
Solid cloud bank 50–
70 km above surface
hiding it from view
Atmosphere is
mostly carbon
dioxide; clouds are
sulfuric acid
The Atmosphere of Venus Venus is the victim of a runaway greenhouse
effect – it just kept getting hotter and hotter as
infrared radiation was reabsorbed
The Surface of Venus
Beta Regio
Alpha Regio
Aphrodite Terra
Chasma region
0° 90° 180° 270°
Ishtar Terra
Lakshmi Planum Maxwell Montes
North The surface is relatively smooth: 60% of
the terrain lies within 500 m of the mean
planetary radius
Two continent-like features: Ishtar Terra
and Aphrodite Terra
No plate tectonics
Mountains, craters, many volcanoes and
large lava flows
The Surface of Venus
Venera 13
photograph of
surface of Venus:
Colors modified
by clouds in
Venus’
atmosphere
The only direct surface information we have about Venus came from
a few Venera spacecraft
Synthetic aperture radar images made by the Magellan spacecraft
give us the greatest detailed information about surface features
After correction for
atmospheric color
effect:
The Surface of Venus Volcanoes on Venus
Above: Sif Mons
Right: Gula Mons
Volcanic Features
on Venus
Baltis Vallis: 6800 km long
lava flow channel (longest
in the solar system!)
Coronae: Circular bulges formed by
volcanic activity
Aine Corona
Lava flows Pancake domes:
Associated with
volcanic
activity forming
coronae
Some lava flows
collapsed after
molten lava drained
away
Craters on Venus
There are nearly
1000 impact
craters on Venus’
surface
Surface not very
old.
There is no water
on the surface; it
has a thick, dense
atmosphere
No erosion
Craters appear
sharp and fresh
Craters of Venus
Venus’ largest
impact crater,
named after
Margaret Mead
Venus’ Magnetic Field and Internal
Structure
There are no measurements available that
would give clues to internal structure.
However, because it is similar to Earth in size
and density, it is reasonable to assume that it
has a similar internal structure.
There is no magnetic field, probably because
its rotation is so slow. This would be
consistent with the magnetohydrodynamic
model.
A History of Venus
Complicated history; still
poorly understood.
Solar wind interacts
directly with the
atmosphere, forming a
bow shock and a long
ion tail.
CO2 produced during
outgassing remained in
the atmosphere (on
Earth: it dissolved in
water).
Any water present on the surface rapidly evaporated
feedback through the enhancement of the greenhouse effect
Heat transport from core mainly through magma flows close to the
surface ( coronae, pancake domes, etc.)
Mars
Earth
Observations
Surface
Features
Volcanism
Craters
Water
Polar Caps
Atmosphere
Satellites
Earth Mars
Semi-major Axis 1 A.U. 1.524 A.U.
Inclination 0° 1° 51’
Orbital period 1.000 tropical year 1.881 tropical year
Orbital eccentricity 0.017 0.094
Rotational period 23 h 56 min 4.1 s 24 h 37 min
Tilt 23° 27’ 25° 12’
Radius 6378 km 3397 km
Mass 5.97 x1024 kg 6.42 x 1023 kg
Bulk density 5.52 g/cm3 3.94 g/cm3
Atmosphere N2, O2 CO2, N2,H2O
Albedo 0.40 0.16
Surface temperature 250-300 K 210-300 K
Escape speed 11.2 km/s 5.0 km/s
Magnetic moment (equator) 8 x 1010 G.km3 2.5 x 107 G.km3
Earth Observations of Mars
Can see polar ice caps that grow and shrink
with the seasons.
Earth Observations of Mars
• Changing polar ice caps are frozen carbon
dioxide (dry ice); water ice is permanently
frozen
• Shifting dust cover makes the surface look
like it is changing
• Frequent dust storms, with high winds
• We did not understand that dust and winds
were responsible for changing features
before spacecraft observations
Orbital Exploration of Mars
1971—Mariner 9
1976—Viking 1 and 2
1993—Mars Observer (failed)
1997—Mars Global Surveyor
2001—Mars Odyssey
2003—Mars Express (ESA)
2006—Mars Reconnaissance Orbiter
No seismic studies have been done
From the behavior of the crust, it is estimated
to be 100 km thick
There is no magnetic field, so the core is
probably not metallic, or not liquid, or neither
liquid nor metallic
Interior of Mars
Surface
Features
Olympus Mons
Tharsis Montes
Elysium Mons
Valles Marineris
Hellas Basin
Chryse Planitia
Argyre Basin
Utopia Planitia
Landing Sites
Curiosity
Phoenix
Surface Spacecraft Exploration
of Mars Viking landers arrived at Mars in 1976.
The Surface of Mars
Both Viking landers landed in low-latitude
northern plains
They
photographed a
rocky surface
The red color is
caused by
hydrated iron
oxides
Viking 1 image
The Surface of Mars Viking 2 image
Shows
frost which
quickly
evaporates
after
sunrise
The Surface of Mars Sojourner rover was deployed on Mars in 1997
during the Pathfinder mission.
The Surface of Mars
Spirit and Opportunity rovers were deployed
on Mars in 2004.
Below is a 360° panoramic image of Spirit’s
landing site
The Surface of Mars
Phoenix landed on
Mars in late May, 2008
and explored the soil
where it landed for ~5
months. It landed
farther north than any
previous Mars
mission. The white
material is water ice.
The Surface of
Mars
Curiosity landed on
August 6, 2012 in 96
mile wide Gale crater.
It will explore the
crater’s central peak,
Aeolis Mons (Mount
Sharp). It is a small
robotic laboratory that
will examine geology
and look for signs of
life.
The Geology of Mars
Giant volcanoes
Valleys
Vallis
Marineris
Impact craters
Reddish deserts of
broken rock,
probably smashed by
meteorite impacts.
The Geology of Mars • Northern hemisphere (left) is rolling volcanic terrain
• Southern hemisphere (right) is heavily cratered
highlands; average altitude 5 km above northern
• Assumption is that northern surface is younger than
southern
• Means that northern hemisphere must have been
lowered in elevation and then flooded with lava
Geology of Mars Northern Lowlands: Free of craters; probably re-surfaced a
few billion years ago. Possibly once filled with water.
Southern Highlands: Heavily cratered;
probably 2 – 3 billion years old.
Volcanism on Mars
Tharsis rise
(volcanic bulge):
Nearly as large
as the U.S.
Rises ~10 km
above mean
radius of Mars.
Rising magma
has repeatedly
broken through
crust to form
volcanoes.
Volcanism on Mars
Volcanoes on
Mars are
shield
volcanoes.
Olympus Mons
Highest and
largest volcano
in the solar
system.
• 700 km diameter
at base
• 25 km high
• Caldera is 80 km
in diameter
The Surface of Mars Impact craters less than 5 km across have mostly been eroded
away
Analysis of areal crater densities allows us to estimate the age of
the surface
The crater on the right may have penetrated a layer of permafrost
that released water and formed the lobate ejecta blankets by
means of fluidized flow.
The Surface of Mars There is evidence of slumping in the wall of this
crater indicating that the surface is probably
covered with unconsolidated material (regolith).
The Surface of Mars Valles Marineris: huge canyon, created by crustal forces
(tectonics)
Grand Canyon on same scale
• 4000 km long
• Maximum 120 km wide, 7 km deep
The Surface of Mars Was there running water on Mars?
Runoff channels
resemble those
on Earth.
Left: Mars
Right: Louisiana
The Surface of Mars
No evidence of a
connected river
system; these features
are probably the result
of flash floods
The Surface of Mars
This may be an ancient
Martian river delta (or
not)
The Surface of Mars
Much of
northern
hemisphere
may have
been ocean
The Surface of Mars Recently, gullies have
been seen that seem to
indicate the presence
of liquid water;
interpretation is still in
doubt
More intriguing, this pair of
images appears to show that
gully formation is ongoing
Hidden Water on Mars
No liquid water permanently on the
surface:
Would evaporate due to low pressure.
But evidence for liquid water in the past:
Outflow channels from sudden,
massive floods
Collapsed structures after withdrawal
of sub-surface water
Splash craters and valleys resembling
meandering river beds
Gullies, possibly from debris flows
Central channel in a valley suggests
long-term flowing water
Evidence for
Water on Mars
Hematite concretions
(spheres)
photographed by Mars
rover Opportunity:
Probably crystals
grown in the
presence of water.
Layered rocks:
Evidence for
sedimentation
Ice in the Polar Caps
Polar caps contains
mostly CO2 ice, but
also water. The water
ice is permanent
Multiple ice regions
separated by valleys
free of ice.
Boundaries of polar
caps reveal
multiple layers of
dust, left behind by
repeated growth
and melting of
polar-cap regions.
The Martian Atmosphere
Martian atmosphere
is mostly carbon
dioxide, and very
thin (~1% of Earth’s
pressure)
95% carbon dioxide
Too thin to retain
much heat;
temperature drops
sharply at night
The Martian Atmosphere
Fog can form in low-lying areas, as sunlight
strikes.
History of Mars’ Atmosphere
Atmosphere probably
initially produced through
outgassing.
Loss of gases from a
planet’s atmosphere:
Compare escape velocity
(red dots) to typical velocity
of gas molecules (blue lines)
The planet was probably
hotter in the past which
would shift the red dots to
the right
Escape velocity less than
gas molecule velocity gas
escapes into space. Mars has lost all lighter gases retaining
only heavier gases (CO2, N2, H2O).
Mars may be victim of an inverse greenhouse.
As water ice froze, Mars became more and more reflective
and its atmosphere thinner and thinner, freezing more and
more water and eventually carbon dioxide as well.
History of Mars’ Atmosphere
History of Mars’ Atmosphere As a result, Mars may have had a thicker atmosphere
and liquid water in the past, but they are now gone
Life on Mars?
Viking landers looked for
evidence of living organisms,
did not find anything
conclusive. Failing to find
carbon using a mass
spectrometer, it was concluded
that the ambiguous results of
three other experiments did
not indicate life.
Life on Mars?
In the mid 1980’s it became evident that some meteorites originated on
Mars. In 1996, scientists claimed to have found evidence for life in an
Antarctic meteorite from Mars. Most planetary scientists are not
convinced that observed features prove that there was life on Mars, but
most believe that conditions on Mars might have supported life at some
point in time (probably not now). We are still looking.
ALH84001
The Satellites of Mars
Phobos (28 km x
20 km)
Deimos (16 km x 10 km)
Mars has two small satellites:
Phobos and Deimos.
They are too small to pull
themselves into a spherical
shape.
Typical of small, rocky, solar
system bodies: cratered,
dusty, dark grey, low density.
Very close to Mars; orbits
around Mars faster than Mars’
rotation.
Both were probably captured from the
inner asteroid belt.