Course astrobiology astronomy Coursera
Astrobiology: Exploring Other Worlds
- Taken on Coursera
- Great visualizations of concepts (eg. doppler shift)
Week 1 - Planets in the Solar System and Beyond
- Astrobiology is asking "are we alone in the universe"?
- There are many planets in the universe but how many of them contain life?
- It's tough to define life
Exoplanets
- Planets beyond our the solar system
- Our situation in cosmic space
- Earth is ~26,000 light years away from the galactic center
- The Milky Way is 100,000 light years in diameter
- The Milky Way is part of a Local Group which is 10 million light years in diameter
- There is nothing special about our place in the Solar System
- A planet is a solid (or partially liquid) body orbiting a star
- Too small to generate energy by nuclear reactions
- Until recently we couldn't see exoplanets directly
- First confirmed exoplanet was 51 Pegasi b
- We have discovered nearly 4000 exoplanets as of 2018
- Many of the first exoplanets were hot Jupiters (close to their star but massive)
- How could they form so close to thier stars?
- Exoplanets tend to have more eccentric orbits than in the Solar System
- Makes us wonder if the Solar System is typical in the universe or not
Planet Formation
- Stars are born in molecular clouds
- These clouds collapse and become dense (gravitational collapse)
- Accretion disk is formed
- Small objects gather and stick together
- The type of exoplanet which a protoplanet will develop into depends where it is positioned in the accretion disk
- Rocky planets
- Inside the frost line
- Available material is primarily rock and dust
- Gas giant planets / ice giant planet
- Outside the frost line
- Protoplanetary disk is mostly ice and gold gas (still has rock and dust)
- Rocky planets
- Differentiation
- Summary
- Molecular cloud collapse
- Protoplanetary disk
- Accretion
- Differentiation
- There are ~100-400 billion stars in the Milky Way
- Some live very short lives
- More long-lived than short-lived
- Recent results from kepler space telescope suggest that between 1/5 to 1/2 of all stars have at least one planet
0.2 * 1000 billion stars = 20,000,000,000
--> conservative estimate is 20 billion stars in the Milky Way
Planets and Moons
- The surface of rocky planets is constantly changing
- Geologically active
- Magnetic shields are a product of differentiation
- Shield the surface from harmful rays of space
- Helps a planet retain its atmosphere
- Planets near their star:
- Hot
- Cannot keep light gasses in their atmospheres
- If they are very close, they tidally lock their star (one side always facing the star)
- Planets far from their star:
- Cold
- May not have liquids on their surface
- Can retain a thick atmosphere
- May have subterranean liquids
- Ices --> mostly frozen hydrogen compounds
- Moons form around planetesimals
- We haven't detected moons around exoplanets
- Too small to detect
Our Solar System
- The Solar System might not be typical but we do believe planet/moon formation is universal
- Planets
- Mercury
- Geologically dead; no atmosphere
- Venus
- Almost identical to Earth in size, mass, and interior structure
- Runaway greenhouse effect
- Might have been habitable 3 billion years ago
- Earth
- Thick atmosphere helps with water retention
- Mars
- Smaller than Earth
- Old, cratered surface
- Evidence it was wet in the past
- Jupiter
- 71% of the mass of all planets in the Solar System
- Saturn
- Uranus
- Large axial tilt (probably from being hit)
- Neptune
- Mercury
Hot Jupiters and Planet Migration
- Hot Jupiter
- gas giant planet with mass equal to, or great than, Jupiter
- Tight orbit close to their parent star
- Surpising that they event exist
- Simulations suggested they should not exist
- Caused us to rethink planet formation theories
- Planetary migration
- The Grand Tack theory
- How Jupiter may have experience planetary migration in our solar system
- Cleared out some debris in the solar system and also caused the period of heavy bombardment
- Extremely hard to verify models of the early solar system
Water Worlds
- Planets like the Earth
- Ice giant planet
- First ice giant exoplanet was discovered in 2014
- Small exoplanets typically come in two sizes
- Measuring mass of planets
- Minimum mass
- Detected using the radial velocity method (Doppler spectroscopy)
- Real orbital inclinations and true masses are generally unkown (sin i degeneracy)
Week 2 - Hunting for Exoplanets
- How do we find exoplanets?
- Small and trillions of miles away
- Two methods for finding
- Wobble observation
- Observing red and blue shift as it moves towards/away from us
- Brightness of its star will dip as it orbits in front
- Wobble observation
Gravity and the Doppler Shift
- Core technique used to find the first exoplanets
- Reflex motion
- Gravitational pull of massive planets (like Jupiter) is enough to exert gravitational influence on their star
- We don't actually see the star move from large distances but observe a red and blue shift
- doppler shift
- Toward us --> blue shift (compressed waves)
- Away from us --> red shift
The Radial Velocity Method
- Uses reflex motion to detect exoplanets
- Magnitude of the Doppler shift indicates the speed of the reflex motion (or radial velocity) of the star
- Limitations
- Limiting mass
- Orbital distance
- Gravitational influence decreases over distance
- Large orbital distances --> barely detectable reflex motion (even for massive planets)
- Only measures mass, not size
- Can't determine orbital inclination
The Transit Method
- Observing the light of a star
- The light will dim as an exoplanet moves in front of the star (transiting)
- Very difficult because the dimming is very short
- Strongly prefers finding hot Jupiters
- Limitations
Learning from Observations
- Relies on Johannes Kepler's laws of planetary motion
- From the radial velocity method:
- With radial velocity and time (radial velocity method) and Keper's first law, we can determine the orbiutal period and distance
- With orbital distance and Kepler's first law, we can calculate the velocity
- Once a planet's velocity is known, we can calculate the mass of an exoplanet
- From the transit method:
- From both:
Planet Composition
- Can be determined from density
- Mass per unit volume of a substance
- Comparative planetology
Microlensing, Imaging, and Selection Effects
- We can't take images of exoplanets because they are too faint compared to their stars
- Coronagraphs
- Gravitational lensing