Title: Announcements
1Announcements
- Passing out marks-so-far today with assignments
- ½ of available marks now given out
- Can always do bonus assignments' (worth 2
credits) - Find current news article relevent to the course
(1 credit) - Briefly describe it and its relevence to the
course (1 credit)
2The Search Mars
- A Short Biography of Mars
- The Planet and its History
- The History of Mars Exploration
- Past
- Current
- Future?
- The Search for (past) Life on Mars
- Viking Experiments
- Microbial Fossils
3A Portrait of Mars as a Small Planet
- Mars
- The atmosphere of Mars
- How it came to be that way
4Mars
- Red planet between Earth and Asteroid Belt
- Half again as far away from Sun as the Earth is
- Expect it to be 100o F colder than Earth on
average - Average too cool for water
- Peak temps 70o F (but -130 at night!)
5Mars
- Near asteroid belt
- Likely more collisions than Earth
- Large impacts can blow off significant rocky
material - Meteorites
- As well as gases (atmosphere)
6Mars
- 1/2 radius of Earth
- 1/10 mass
- 40 surface gravity
- Force of a 1 lb weight less than ½ lb on Mars
- Less gravity holding the atmosphere in place
7Mars
- Too little gravity to be able to hold onto a
significant atmosphere - Atmospheric pressure less than 1 of Earth's
8Evaporation
- What causes evaporation of liquid, and what
prevents it?
9Evaporation
- What causes evaporation of liquid, and what
prevents it? - Fastest moving water (say) molecules can escape
into atmosphere - Water molecules in atmosphere can collide into
water and become part of the liquid - Balance is reached when evaporating water
condensing water
10Evaporation
- Can change balance
- Little water in atmosphere, evaporation happens
faster - (Why feel so sticky on a humid day)
- If air pressure is very low, evaporated water
molecules can move very far away from pool of
water - Fewer around to condense
- Faster evaporation
11Evaporation
- Effect of atmospheric pressure happens on our own
planet - Reason for high-altitude cooking instructions'
on some boxes - Higher altitude -gt lower air pressure -gt
evaporation is easier -gt lower boiling point
12Evaporation
- Martian atmospheric pressure lt 1 of Earth's
- (Earth's atmosphere at 15 miles / 80,000 ft)
- Water boiling point is so low that any liquid
water evaporates immediately - No free water possible on surface
13Evaporation
- But water ice DOES exist on Mars
- Polar ice caps
- Mostly (on top) dry ice (frozen CO2)
- Underneath, visible when CO2 has sublimated,
water ice - Quite likely some trapped under surface
permafrost'
14Atmospheric Pressure
- Atmospheric pressure is seasonal
- Dry ice caps melt
- Increase CO2 in atmosphere
- Increase atmosphere pressure
- Dry ice caps re-freeze
- Pressure decreases
15The Reasons for the Seasons
- Earth's (and Mars') axis is tilted
- Earth 23.5o (Mars 25.9o)
- Tilt stays in same direction as planet orbits Sun
16The Reasons for the Seasons
- Sun comes in at different angle when planet is at
different positions - Summer
- Light most direct
- Sun closest to being overhead
- Winter
- Comes in at angle
- Same amount of light covers larger area
- Increased reflection
Summer
Winter
17The Reasons for the Seasons
Fall Cubs win (effective 2003)
- Orientation changes over course of year
- Another effect Earth is slightly further from
Sun in (Northern Hemisphere) Winter than in
Summer - Only 1 effect (5oF)
- Effect of orientation 16 effect (90oF)
Winter Bears Lose
Spring Bulls Lose
18Ecliptic
- Because of Earth's tilt, equator (and rotation)
do not line up with plane of the solar system - Solar system objects (Sun, Moon, planets) apear
to lie along an arc ecliptic
19Ecliptic
- Planets are along plane of solar system
- Appear on Earth to along an arc
- Mars visible these days early at night towards
the East, even from Chicago - Bright reddish star'
- Near a bright greenish-yellow star' (Venus)
Starmap for tonight, 9pm
20How Mars Came to Be This Way
Large Enough for Atmosphere
- Distance from Sun makes global liquid water
difficult but not impossible - NO ATMOSPHERE
- Liquid water quickly evaporates
- No greenhouse effect to warm planet, regulate
temp. - No ozone to protect from UV
Not Large Enough for Atmosphere
21The History of Martian Exploration
- Past explorations
- Current Rover Missions
- Future Plans
22Exploration of Mars Today
- So many recent missions to Mars that it's
becoming almost anticlimatic - News filled with discoveries from current rovers
- Still very difficult
- Success rate low!
- Scientists can't go there at whim yet
23Observations of Mars from Earth
- Early telescope observations
- observations' of canals
- Improved telescopes showed this not to be the
case - Later, radio observations
- Surface temperature
- Crude radar maps of surface
241960-2 Korabl (Marsnik')
- Attempted Russian Probes
- 4 attempted flybys, 1 attempted landing
- Most barely made it past Earth orbit, one was
lost between Earth and Mars
251964 Mariner, Zond
- Mariner 3, 4 (USA) attempted flyby
- Mariner 3 Couldn't make it to Mars
- Mariner 4 First flyby, close up pictures
- Zond 2 (USSR) Russian flyby, descent
- Lost on its way to Mars
261969 Mariner, Mars 1969
- Mariner 6,7 Identical flyby craft
- Mariner 4 First flyby, close up pictures
- Mars 1969A/B Russian flyby, descent
- Didn't survive takeoff
271971 Mariner, Mars 2/3 Orbiters
- Mars 2/3 (USSR) First orbiter of another world
- Measured temps, magnetic fields
- Sent probe, 1 crashed too fast, other survived 20
hours Mariner 8 didn't make it - Mariner 9 Orbited, obscured by storms
- First close-up views of moons of Mars
281973 Mars 4/5/6/7 (USSR)
- Mars 4 Brakes didn't work flew by instead of
orbited - Mars 5 Successful Orbit, pictures
- Mars 6 Descent, sent data from atmosphere
before shutting down, but data garbled - Mars 7 Missed Mars entirely
291975 Viking 1,2 (USA)
- Identical Orbiter lander
- Orbiters searched for safe landing places
- Extensive weather measurements, chemistry/biology
experiments - Sent several thousand images, data
301988 Phobos 1,2 (USSR)
- Lost due to human error (Phobos 1), computer
malfunction (Phobos 2)
311988-1992
- 1988 Phobos 1, 2 (USSR)
- Lost due to human error (Phobos 1), computer
malfunction (Phobos 2) - 1992 Mars Observer (USA)
- All contact lost 3 days from Mars
32Very Recent Mars Missions
- 1996
- Mars 96 (USSR) Didn't successfully leave Earth
- Mars Global Surveyor (USA)
- Looking for places to send Pathfinder
- Still sending back data
- Mars Pathfinder
- Probe with some sensors
- Test of new technologies, techniques
331998 Less Successful
- Nozomi (Japan)
- Navigation problems
- Could not reach Mars at expected time
- Unable to orbit Mars
- Mars Climate Orbiter (USA)
- Crashed into Mars after mistake in converting
units in probe computer programming
341998-9 Less Successful
- Nozomi (Japan)
- Navigation problems
- Could not reach Mars at expected time
- Unable to orbit Mars
- Mars Climate Orbiter (USA)
- Crashed into Mars after mistake in converting
units in probe computer programming - Mars Polar Lander (USA)
- Signal lost near Mars Navigation errors?
352001 Mars Odyssey(NASA)
- Orbiter
- Build global map of telements, minerals on the
Mars surface - Determine the abundance of hydrogen in
subsurface. -gt hidden deposits of water ice? - Structure of the Martian surface.
- Radiation environment between the Earth and Mars
and in low Mars orbit (radiation-related risk to
human exploration) - Communication relay Spirit/Opportunity/Beagle
362001 Mars Express(Europe)
- Orbiter Lander/Rover (Beagle)
- Beagle lost
- Image globe in 3D
- Build accurate picture of meteorology/climage
- Communications Relay
372003 Spirit, Opportunity(USA)
- Search for/study many types of rocks and soils
that might hold clues to past water activity. - Maps showing the locations of different kinds of
rocks and soils around the landing sites. - What forces have shaped the landscape
- Search for minerals that contain water/formed in
water. - Identify minerals, how made
- Clues to what environment was like in past
38The Search for Life on Mars
- Pictures of surface
- Viking biology experiments
- Meteoritic fossils'
- Future?
39Venus
- Closest to Earth
- ¾ as far away from Sun as Earth is
- Very similar to Earth's size, density
- Covered by thick, opaque clouds
40Reading for Next Class (Apr 16)
- Chapter 15 The Outer Solar Systen
- History of Outer Solar System Exploration
- The Nature of Gas Giants
- Atmosphere
- Chemistry
- The Moons of Jupiter, Saturn, Uranus, Neptune
- Chapter 16 How Unique is Earth?
- Necessary Resources
- On Having a Large Moon
- Staying alive by accident