Section 3 - Habitable
Zones and Extra-Solar Planets
Study: Chapters 10 and 11
Chapter 10
General question:
What determines the "suitable zones" where life might exist on planets,
in terms of the properties of the central star and the conditions on
the planet.
What do we mean with suitable conditions?
Main criterion: Temperature
on the planet such that water may exist in liquid form.
Other factors:
a. radiation conditions: too much UV light may be bad, depending on the
planet's capability to shield the surface from UV light. So the
atmosphere of the planet will matter for this too.
b. For how long will the
conditions be suitable? If Earth is typical,
it has taken a long time to develop advanced life forms here. We therefore need to study how
long different stars can shine.
The factors that enter the life times of stars are:
How luminous and hot is the
star; stars emit more light the larger and/or hotter they get.
The radiation emitted by a hotter and more luminous star has more
energy to heat planets further away from the star than for a less
luminous star. In general,
the amount of light intercepted by a planet decreases as the inverse of
the distance squared to the star. This is simply a consequence
of energy conservation: the light from the star is spread out over a
larger area and volume as it moves away from the star.
The temperature on the planet or moon
depends on several factors:
- amount of energy received as light from the
central star
- how reflective is the planet? If it is very
reflective, more of the star light will be bounced back into
space and the planet will be colder. We call the reflectivity the
"albedo". A "black body" is the most efficient absorber of light.
- properties of the atmosphere (greenhouse effect)
- rotation rate of planet (will affect difference
between day/night side temperatures, as does the greenhouse
effect)
- other heat sources: internal or external (e.g.
tidal forces on moons). Even if it is too cold in terms of solar
radiation near Jupiter and Saturn, there can still be moons with
liquid water, providing a possible local habitable zone.
- angle of incidence of sunlight; tilt of rotation
axis. This does not affect how much heat the entire planet
gets from the star, but it will affect climates and weather
patterns on the planet and cause seasons if the rotation axis is not
perpendicular to the orbital plane.
How large is the habitable zone in the Solar System? We
call the
distance between Earth and Sun 1 Astronomical Unit. Is the habitable
zone 0.5-1.5 Astronomical Units? Or 0.95-1.05 A.U? Venus is too
hot, Mars perhaps too cold. There may also be habitable zones around
some of the giant planets, as we saw.
Some features of Venus:
Venus is the planet with the most extreme greenhouse effect in the
solar system, due to its thick atmosphere. What happened to the water
that likely was once present on Venus? Likely lost to space as any
surface water molecules evaporated into the atmosphere and were
dissociated there due to the Sun's UV light (which is more intense near
Venus than Earth).
Changes in solar system's
habitable zone over time:
The Sun's energy output is gradually climbing from its early days of
hydrogen fusion to the present. This general increase in brightness
(measured in percentages, roughly 30% or so) is very important but
happens very slowly so it is not something we need to worry about now.
It implies the habitable zone was closer to the Sun in the past and is
slowly moving outward.
A more dramatic change comes about when the Sun has exhausted the
hydrogen in its core available for nuclear fusion. The center will
shrink and heat up a lot, while the other layers will swell to enormous
size. Eventually, in the center, helium will fuse into carbon. The
Sun's luminosity will increase by factor of a 100, its diameter by a
factor of a 100. The color of the Sun will turn redder, as it is cooler
in the outer atmosphere. However, the higher luminosity will greatly
increase temperatures throughout the solar system, with Earth getting
warmer than 700 C. The luminous phase of the sun will last a billion
years, and then it will expell its outer layers and slowly cool as a
white dwarf.
Stars
like sun expelling their outer atmosphere, hourglass nebula
another
example: stingray nebula
Ok,
one more: Eskimo nebula
While
the sun itself will fade to a white dwarf
Thus the long time fate of the solar system is darkness and cold
temperatures. A similar fate awaits the universe as a whole, as it
keeps expanding and gradually converts any remaining gas clouds in
stars with cold stellar remnants left at the end. This is many, many
billions of years in the future.
Properties of stars relevant to how
large their habitable zones may be and how long the stars can shine.
Stars other than Sun:
- Realization that stars are like our Sun, but more distant.
A
Milky Way full of stars and dust: direction towards the Galactic Center
And in a bit more
detail
- Measure distances to stars: simplest method is the parallax. Works
only for relatively nearby distances.
Diagram
to explain parallax
- Not all stars are same: we see stars of different apparent and
intrinsic brightness, and different color.
What causes these
differences?
Why do we care about it?
What kind of stars exist in galaxies. Are all stars like the Sun? Can
all stars shine as long as the Sun? The answer is definitely NO to
these questions. However, there are also very many stars like the Sun
in the MW.
If stars are different from the Sun, how does that affect their
habitable zone? There are several important effects to consider:
- hotter stars emit more
UV light which may affect development of life on
planets
- many stars are much more luminous than the Sun pushing
their habitable
zone away from the star
- many stars are much cooler which would imply the
habitable zone is
likely much closer to the star
- hot, luminous stars, as we will see, can not shine
very
long. Therefore,
their habitable zone is also limited in the time available to develop
life.
- Low luminosity small stars can shine much longer than
the Sun and could
still support life possibly since there is much time available.
Useful relations/knowledge learned about stars which
taught us all these things:
- Luminosity-color relation: Herzsprung-Russell
diagram. A plot of stellar temperature (color) versus stellar luminopsit
HR
diagram of an old globular star cluster
- Mass-Luminosity relationship (related to how long
stars can shine)
- Evolutionary stage of stars (Main Sequence phase
versus post-MS evolution).
We have learned an enormous amount of information on how
stars evolve and how they shine by study of star clusters. In the Milky
Way and in other galaxies we find close groups of stars. We distinguish
two types:
- open clusters
are losely bound groups of hundreds of stars, We find them at all ages
in the MW.
Pleiades
open star cluster: blue stars, more massive than Sun and hundreds of
fainter members
Old
open cluster NGC 6791
- globular
clusters are very dense groups of stars with 10,000 to 100,000
members. The age of globular clusters is old.
Globular
cluster 47 Tucanae
Hubble Space
Telescope photograph of globluar cluster M15
There are two special properties that make study of star clusters so
useful:
1. The stars in a
cluster are all at the same distance from us. That way we can directly
study brightness variations among stars and deduce that not all stars
are the same or can shine for equally long times.
2. The stars in a cluster must have formed at the same
time since the chance of forming a cluster of stars by random
encounters of stars is negligible. By studying star clusters at
different ages we can therefore infer how stars evolve over time.
Hr
diagram of an old cluster
HR
diagram for several clusters: see how it changes with age of the cluster
Explanation of the
Mass-Luminosity relationship for stars.
Goal: we
are trying to understand how long various stars can shine, so
how long they can generate energy through nuclear fusion in their core
and stay hot. This is a simple matter of supply and demand: how
much
energy can the star generate, and how fast is it losing energy through
the light that it emits.
First an example. A pickup truck has a 40 gallon tank and gives
10 miles/gallon on average. A civic hybrid has an 11 gallon tank and
gives 50 miles/gallon on average. Which car can go further on one tank?
How did you calculate this?
When you study this problem, you will see that you take the energy
supply (equals gas in the tank in gallons) and multiply that by the
miles/gallon figure to see how many miles you can go. We can re-state
this problem, by giving the energy consumption per mile rather
than the miles/gallon. In that case we get for the pickup that it needs
0.1 gallons per mile, and it can travel:
40 gallons divided by (0.1 gallons/mile) = 400 miles.
Now, let's go back to stars. For stars, the available energy supply is
a fraction of the star's mass, namely that fraction that is converted
into energy through E=mc2. The rate at which energy is being
used is the "luminosity" = "power" of the star. How long can a star
last then? That is given by:
available energy supply
divided by energy loss rate; this is proportional to the mass of the
star divided by the stellar luminosity. The unit you get when you do
this calculation is a unit of time, as it should be.
Here comes the interesting
part: massive stars produce far more luminosity than low-mass
stars. The relationship is not linear (in which case all stars would be
able to shine equally long) but cubic, that is, the luminosity of a
star scales as the mass to the power 3. The net result is that a star
that is, say, 10 times more massive than the Sun will use up its total
energy
100 times faster than the Sun, so it will only shine 1/100th of the
time the Sun can shine, and a star that is 100 times more massive will
only be able to shine for 10,000 less long than the Sun before it runs
out of energy.
Conclusion: if life takes billions of years to develop to fairly
advanced stages around stars like the Sun, very massive stars are
unlikely to be good places to look for planets with life. A massive
star's life is measured in millions of years, rather than billions of
years.
Galaxies like our Milky Way contain many stars like the Sun, fewer
massive stars, and many more low-mass stars. The low-mass stars will be
cooler than our Sun but can shine much longer and they may be good
places to look for planets and life.
Another interesting bit of information: as much as 50% of all stars may
be occuring in binary systems, that is, two stars orbiting around each
other. We also call them double stars. Some systems have 3 or even more
stars orbiting each other. Finding planets is a bit like finding binary
star systems, except much harder.
Chapter 11
DETECTING
PLANETS AROUND OTHER STARS
The last planet in our solar system was discovered in 1930 (ignoring
the debate of whether it is a planet!). It has
taken about another 65 years since then to find the first solid
evidence for planets around other normal stars. Why is it so hard to
find planets around other stars?
- The stars are bright, the planets are faint! Here is how hard this is:
The closest star to us other than the Sun is 4 light years away. This
star's brightness as seen by us is about the same as that of a 150
Watts lightbulb at a distance of 15 miles away from us. On this scale
of 15 miles distance, the Earth would be a dust speck much smaller than
a mm. It would be about 10 cm away from the lightbulb. Imagine trying
to detect a dust speck that is next to a 150 Watts light bulb from a
distance of 15 miles away. That is how hard it is to detect Earth sized
planets around stars. How about Jupiter? Jupiter would be about 50 cm
away from the lightbulb, and still be at least a billion times fainter
than the light bulb.
It has been possible to find binary (=two) star systems, since
both stars are visible if they are not too close to each other.
If this seems hopeless for planets, it is by and large (although future
imaging techniques will
allow detection of these planets through images) and most of the
planets now
known to exist around other stars have been discovered in other ways,
that are essentially methods similar to those how most close
binary star systems have been found. The situation is slightly better
for large planets and dim, cool stars, where a few images of the
star-planet system have now been obtained.
a. Through "occultations",
or "transits".
The planet moves in front of the star, and temporarily
dims the light. What is required for this? How much would star light be
dimmed?
Transiting
extrasolar planet light curve for star HD149026b.
The answer is quite simple. From our perspective, the distant star and
its planet are about equally far away. Thus, the planet will cover a
fraction of the area of the star that is equal to the ratio of the area
of the planet to the area of the star:
(planet diameter)2/(star
diameter)2. In the case of a planet like Jupiter, it would
block about 1% of the star's light in the transit, while a planet like
Earth would only block 0.01% of the star's light; with modern
instruments we
can detect the 1% dip easily, while the 0.01% dip is very difficult to
measure.
b. Through motion of star.
If you can't see the planet, look for the effect of the planet's motion
on the star: the star wobbles due to force of gravity exerted
on it by the planet. The wobble can be detected in star's velocity.
What would the size of the wobble depend on? How fast would it
wobble?
The star wobbles at the same rate as the planet completes an orbit. It
is easiest to imagine this as having two stars of equal mass orbiting
each other. In that case, intuition tells us the stars would be moving
at the same rate and would always be opposite each other in their
orbit. Newton's laws can be used to show that this intuition is right.
In the case of objects of very
different mass, the speeds of the two objects vary inverse to their
mass, but the two objects still each complete their orbit in the same
time. The orbit of the more massive object is just much smaller than
the orbit of the less massive object (which is why Kepler concluded
that the Sun was at rest; it isn't, but it's motion is very small).
An example:
If the star is 1000 times more massive than the planet, the star's
velocity in its orbit will be 1000 less than the planet's velocity. A
planet like Jupiter is about 1000 times less massive than the Sun.
Jupiter orbits at 750,000,000 km from the Sun, and completes one orbit
in 11 years. As a result of Jupiter's motion around the Sun, the Sun
completes its own little orbit in 11 years, and the radius of the orbit
is 1000 times less than that of Jupiter, so 750,000 km, which is about
equal to the radius of the Sun.
- Kepler was wrong: stars are not at rest in the
ellipse.
- How to detect the wobble?
Doppler effect shifts
light to bluer colors
when star approaches us, and to redder
colors
when star is moving away from us. We can detect this!
Question: why not observe the Doppler effect for the planet which moves
faster?
Illustration
of Doppler technique for detecting binary stars (scroll down the
page to see animation).
Look at the above animation. What would be different for planet?
(answer: you would detect the tiny motion of the central star, not the
large motion of the small planet!). In reality, the situation is more
complex. The stars spectrum has dark absorption lines that we can
measure the blue and red shift of. However, stars can also pulsate on
their own and astronomers have to be very careful to rule out other
causes of the shifting of the lines.
astrometry: in principle, we can
also detect the motion of the star as a wobble on the sky compared
to other
distant stars. This has been tried in the past, but the motion is so
small it is difficult to detect. Still, this will be an important
technique in the future as our accuracy in imaging improves. Many
double stars have been found this way.
c.
A third technique: through gravitational
lensing. The light from background stars can be amplified by a
foreground system, causing a star to vary systematically in brightness.
If the foreground system has planets, the light variations may be
different. Here is an example:micro lensing by
a star with a planet
Can we take pictures of the planets that have been discovered: mostly,
not yet, but in the future yes, although they will be tiny pictures
with not any detail. Coronographic techniques are used to block the
star light as best as possible. Scattered light is a problem, so we
need to go outside the Earth's atmosphere and use clever imaging
techniques in space to block the light of the star.
What is the problem with
finding Earth sized planets?
Both principle detection techniques (Doppler shift and occultations)
produce weakest signal for low mass planets or for planets far away
from the star. So, the planets that have been found are typically
close to the star and massive. This was surprising (since people
thought you could not form Jupiter size planets close to a star) but we
have to keep in mind that there is a strong bias here, since those are
the ones that can be most easily found.
What has been discovered about the extra-solar planets thus far:
- on average, in about 10% of stars more or less like the Sun planets
have been found. The other 90% may have planets, but detection limits
may not yet be good enough to find them
Question: can we find planets if we would see the star/planet system
from above (vertical to the orbital plane)?
- Many stars have multiple planets. The ability to detect multiple
planets relies on very well measured Doppler shifts for the stars
(and/or patience to detect eclipses of the star by the planets!)
- Planets with mass of Earth have been found, but in a surprising
place: surrounding neutron stars! These are the only objects were
current techniques allowed detection of such low mass planets.
Challenge in measuring the masses of planets: inclination of the orbit
not known unless it eclipses the star.
- Some knowledge of planetary atmospheres has been found too, with
Hubble Space Telescope, where sodium was detected in planet's
atmosphere. This technique shows great promise for future. It relies on
change in star's spectrum during an eclipse by the planet.
- Planets have also been found in binary star systems!
Planet searches, wrap up:
Current
list of planets detected (Note that the masses are in Jupiter
masses, except as noted). The most unexpected place to find them. Click
on planet's and star's names and you get an overview of what these
objects are and where they are.
The most peculiar objects in this list are the candidates found near a
pulsar (labeled PSR in the list).
Techniques:
- transits to detect temporary and periodic dimming of starlight
- Detecting the wobble of the star resulting from the presence of the
planet(s):
Dopper shift in
velocities detected in light from star, could be in normal stars or in
neutron star (= pulsar) where we detect Doppler shift in the frequency
of the pulses of radio emission
- Gravitational lensing ("micro lensing") of
normal stars, where we look for light variations in star due to lensing
of background object. Presence of planet may give different light
variation. Drawback: one time even for each star!
Results:
- Planets with mass of about Earth only found so far around neutron
star, but planets with just 10 or so times the mass of Earth found
around normal stars with Doppler technique, only possible if they are
very close to the star.
- Many planets found, sometimes multiple per star, up to as many as 4
per star.
- Results biased towards detecting massive planets close to stars; a
large part of the search space cannot yet be explored (e.g. Earth size
planets or large planets very far from star)
comparison
of extra-solar planets with solar system planets
- Stars with higher abundance of "heave elements" (anything above
Helium) have higher chance of having planets detected around them.
Here is a great
link about extra-solar planets, courtesy of JPL and NASA
Future
plans for finding smaller planets (click on Interactive Flash
overview)
Is the Earth unusual? The "rare Earth hypothesis"
See section 11.3 in book.
Are conditions on Earth so special that it is likely few planets will
exist that are like Earth?
a. Requirement for high abundance of heavy elements to form rocky
planets. Likely not an issue, since most of the Galactic disk has
abundance of heavy elements like Sun or higher.
b. Requirement for avoiding major impacts from occuring too frequently.
Jupiter plays a critical role in keeping the asteroid belt where it is
(between Mars and Jupiter and not crossing Earth's orbit). Also, most
of comets are far from Sun in comet cloud, but they may have been
formed much closer in, in region where major gas giants formed. Again,
the massive planets are responsible for sweeping them to the outer
orbits. The Moon may also play some role in the impact rate of
asteroids and comets on earth.
Does every Earth need a Jupiter in the right place so that life has
enough time to form and evolve?
We don't know enough to be sure of this. But it surely is no problem to
form Jupiter size planets as the extra-solar planet results thus far
show.
c. Is a stable climate rare?
The stability of the Earth's climate may be related to the Earth's
ability to regulate the amount of natural greenhouse gases (notably
CO2) in the atmosphere. Plate tectonics plays an important role in this
cycle.
A second important factor is the presence of the Moon. The Moon is
responsible for keeping the Earth's tilt at a pretty constant angle.
There is some evidence that Mars's axis shows much larger variations in
the tilt over long periods. The likely formation mechanism for the Moon
is a giant impact of a mars-sized object with Earth early in the
formation of the solar system. The Earth is not massive enough on its
own to attract enough matter to form large moons like the gas giants
did. Thus, the presence of the Moon could be quite rare.
We don't know though, if a variation in tilt axis would preclude
development of (advanced) life.
In balance, "reasoning after
the fact ("a posteriori") always can seem to point at magical
coincidences for certain events to happen. But that is a dangerous
thing to do from a scientific perspective. It is much better to get
real data on the variation of planetary systems and from there draw the
conclusions what is required for life and what is rare or common.