Any
planet is an extremely faint light source
compared to its parent
star. In addition to the
intrinsic difficulty of detecting such a faint light source, the
light from the parent star causes a glare that washes it out. For
thosereasons, only a very few
extrasolar planets have been observed
directly.
Instead, astronomers have generally had to resort to indirect
methods to detect extrasolar planets. At the present time, several
different indirect methods have yielded success.
Established detection methods
Astrometry
This method consists of precisely measuring a star's position in
the sky and observing how that position changes over time.
Originally this was done visually with hand-written records. By the
end of the 19th century this method used photographic plates,
greatly improving the accuracy of the measurements as well as
creating a data archive. If the star has a planet, then the
gravitational influence of the planet will cause the star itself to
move in a tiny circular or elliptical orbit. Effectively, star and
planet each orbit around their mutual center of mass (
barycenter), as explained by solutions to the
two-body problem. Since the star is
much more massive, its orbit will be much smaller. Frequently, the
mutual center of mass will lie within the radius of the larger
body.
Astrometry is the oldest search method for
extrasolar planets and originally popular
because of its success in characterizing
astrometric binary star
systems. It dates back at least to statements made by
William Herschel in the late 18th century.
He claimed that an
unseen companion was affecting the
position of the star he cataloged as
70
Ophiuchi. The first known formal astrometric calculation
for an extrasolar planet was made by
W.
S. Jacob in
1855 for this star. Similar calculations were repeated by others
for another half-century until finally refuted in the early 20th
century.For two centuries claims circulated of the discovery of
unseen companions in orbit around nearby star systems that
all were reportedly found using this method, culminating in the
prominent 1996 announcement of multiple planets orbiting the nearby
star
Lalande 21185 by
George Gatewood. None of these claims
survived scrutiny by other astronomers, and the technique fell into
disrepute. Unfortunately, the changes in stellar position are so
small and atmospheric and systematic distortions so large that even
the best ground-based telescopes cannot produce precise enough
measurements. All claims of a
planetary companion of less
than 0.1 solar mass (a planet) made before 1996 using this method
are likely spurious. In 2002, however, the
Hubble Space Telescope did succeed in
using astrometry to characterize a previously discovered planet
around the star
Gliese 876.
Future space-based observatories such as NASA's
Space Interferometry Mission
may succeed in uncovering large numbers of new planets via
astrometry, but for the time being it remains a minor method of
planetary detection.
One potential advantage of the astrometric method is that it is
most sensitive to planets with large orbits. This makes it
complementary to other methods that are most sensitive to planets
with small orbits. However, very long observation times will be
required — years, and possibly decades, as planets far enough
from their star to allow detection via astrometry also take a long
time to complete an orbit.
In 2009 the discovery of
VB 10b by astrometry
was announced. This planetary object was reported to have a mass 7
times that of
Jupiter and orbiting the
nearby low mass
red dwarf star
VB 10. If confirmed, this will be the first exoplanet
discovered by astrometry of the many that have been claimed through
the years.
Radial velocity
Like the astrometric method, the radial-velocity method uses the
fact that a star with a planet will move in its own small orbit in
response to the planet's gravity. The goal now is to measure
variations in the speed with which the star moves toward or away
from Earth. In other words, the variations are in the radial
velocity of the star with respect to Earth. The radial velocity can
be deduced from the displacement in the parent star's
spectral lines due to the
Doppler effect.
The velocity of the star around the
center of mass is much smaller than that of
the planet because the radius of its orbit around the center of
mass is so small.
Velocity variations down to 1 m/s can be
detected with modern spectrometers,
such as the HARPS (High Accuracy
Radial Velocity Planet Searcher) spectrometer at the ESO
3.6 meter
telescope in La Silla
Observatory
, Chile, or the HIRES spectrometer at the Keck telescopes
.
This has been by far the most productive technique used by planet
hunters. It is also known as Doppler spectroscopy. The method is
distance independent, but requires high
signal-to-noise ratios to achieve high
precision, and so is generally only used for relatively nearby
stars out to about 160 light-years from Earth. It easily finds
massive planets that are close to stars, but detection of those
orbiting at great distances requires many years of observation.
Planets with orbits highly inclined to the line of sight from Earth
produce smaller wobbles, and are thus more difficult to detect. One
of the main disadvantages of the radial-velocity method is that it
can only estimate a planet's minimum mass. Usually the
true mass will be within 20% of this minimum
value, but if the planet's orbit is almost perpendicular to the
line of sight, then the true mass will be much higher.
The radial-velocity method can be used to confirm findings made by
using the
transit method. When both
methods are used in combination, then the planet's true mass can be
estimated.
Pulsar timing
A
pulsar is a neutron star: the small,
ultradense remnant of a star that has exploded as a
supernova. Pulsars emit radio waves extremely
regularly as they rotate. Because the intrinsic rotation of a
pulsar is so regular, slight anomalies in the timing of its
observed radio pulses can be used to track the pulsar's motion.
Like an ordinary star, a pulsar will move in its own small orbit if
it has a planet. Calculations based on pulse-timing observations
can then reveal the parameters of that orbit.
This method was not originally designed for the detection of
planets, but is so sensitive that it is capable of detecting
planets far smaller than any other method can, down to less than a
tenth the mass of Earth. It is also capable of detecting mutual
gravitational perturbations between the various members of a
planetary system, thereby revealing further information about those
planets and their orbital parameters.
The main drawback of the pulsar-timing method is that pulsars are
relatively rare, so it is unlikely that a large number of planets
will be found this way. Also, life
as we know it could not
survive on planets orbiting pulsars since high-energy radiation
there is extremely intense.
In 1992
Aleksander Wolszczan
and
Dale Frail used this method to
discover planets around the pulsar
PSR
1257+12. Their discovery was quickly confirmed; making it the
first confirmation of planets outside our
Solar System.
Transit method

Transit method of detecting extrasolar
planets.
The graph below the picture demonstrates the light levels
received over time by Earth.
While the above methods provide information about a planet's mass,
this
photometric method can
determine the radius of a planet. If a planet crosses (
transits) in front of its parent star's
disk, then the observed visual brightness of the star drops a small
amount. The amount the star dims depends on the relative sizes of
the star and the planet. For example, in the case of
HD 209458, the star dims 1.7%.
This method has two major disadvantages. First of all, planetary
transits are only observable for planets whose orbits happen to be
perfectly aligned from astronomers' vantage point. The probability
of a planetary orbital plane being directly on the line-of-sight to
a star is the ratio of the diameter of the star to the diameter of
the orbit. About 10% of planets with small orbits have such
alignment, and the fraction decreases for planets with larger
orbits. For a planet orbiting a sun-sized star at 1
AU, the probability of a random alignment
producing a transit is 0.47% However, by scanning large areas of
the sky containing thousands or even hundreds of thousands of stars
at once, transit surveys can in principle find extrasolar planets
at a rate that could potentially exceed that of the radial-velocity
method , although it would not answer the question of whether any
particular star is host to planets.
Secondly, the method suffers from a high rate of false detections.
A transit detection requires additional confirmation, typically
from the radial-velocity method.

Properties (mass and semimajor axis)
of planets discovered using the transit method, compared (light
gray) with planets discovered using other methods.
The main advantage of the transit method is that the size of the
planet can be determined from the lightcurve. When combined with
the radial velocity method (which determines the planet's mass) one
can determine the density of the planet, and hence learn something
about the planet's physical structure. The nine planets that have
been studied by both methods are by far the best-characterized of
all known exoplanets.
The transit method also makes it possible to study the atmosphere
of the transiting planet. When the planet transits the star, light
from the star passes through the upper atmosphere of the planet. By
studying the high-resolution stellar spectrum carefully, one can
detect elements present in the planet's atmosphere. A planetary
atmosphere (and planet for that matter) could also be detected by
measuring the polarisation of the starlight as it passed through or
is reflected off the planet's atmosphere.
Additionally, the secondary eclipse (when the planet is blocked by
its star) allows direct measurement of the planet's radiation. If
the star's
photometric
intensity during the secondary eclipse is subtracted from its
intensity before or after, only the signal caused by the planet
remains. It is then possible to measure the planet's temperature
and even to detect possible signs of cloud formations on it. In
March 2005, two groups of scientists carried out measurements using
this technique with the
Spitzer
Space Telescope.
The two teams, from the Harvard-Smithsonian Center for
Astrophysics
, led by David
Charbonneau, and the Goddard Space Flight Center
, led by L. D. Deming, studied the planets
TrES-1 and
HD
209458b respectively. The measurements revealed the planets'
temperatures: 1,060
K (790°
C) for TrES-1 and about 1,130 K (860°C) for HD
209458b.
In addition the hot Neptune Gliese 436 b enters secondary eclipse. However some transiting planets orbit such that they do not enter secondary eclipse relative to Earth; HD 17156 b is over 90% likely to be one of the latter.
A
French Space Agency mission,
COROT, began in 2006 to search for planetary transits
from orbit, where the absence of atmospheric
scintillation allows improved
accuracy. This mission was designed to be able to detect planets "a
few times to several times larger than Earth" and is currently
performing "better than expected", with two exoplanet discoveries
(both "hot jupiter" type) as of early 2008.
In March 2009,
NASA
mission Kepler was
launched to scan a large number of stars in the constellation
Cygnus with a measurement
precision expected to detect and characterize Earth-sized
planets. (see section on
Observations from space below).
Gravitational microlensing

Gravitational Microlensing
Gravitational microlensing occurs when the gravitational field of a
star acts like a lens, magnifying the light of a distant background
star. This effect occurs only when the two stars are almost exactly
aligned. Lensing events are brief, lasting for weeks or days, as
the two stars and Earth are all moving relative to each other. More
than a thousand such events have been observed over the past ten
years.
If the foreground lensing star has a planet, then that planet's own
gravitational field can make a detectable contribution to the
lensing effect. Since that requires a highly improbable alignment,
a very large number of distant stars must be continuously monitored
in order to detect planetary microlensing contributions at a
reasonable rate. This method is most fruitful for planets between
Earth and the center of the galaxy, as the galactic center provides
a large number of background stars.
In 1991,
astronomers Shude Mao and Bohdan
Paczyński of Princeton University
first proposed using gravitational microlensing to
look for exoplanets. Successes with the method date back to 2002,
when a group of Polish astronomers (Andrzej Udalski, Marcin Kubiak
and Michał Szymański from Warsaw
, and Bohdan
Paczyński) during project OGLE (the Optical Gravitational
Lensing Experiment) developed a workable technique.
During one month they found several possible planets, though
limitations in the observations prevented clear confirmation. Since
then, four confirmed extrasolar planets have been detected using
microlensing. this is the only method capable of detecting planets
of Earthlike mass around ordinary
main-sequence stars.
A notable disadvantage of the method is that the lensing cannot be
repeated because the chance alignment never occurs again. Also, the
detected planets will tend to be several kiloparsecs away, so
follow-up observations with other methods are usually impossible.
However, if enough background stars can be observed with enough
accuracy then the method should eventually reveal how common
earth-like planets are in the galaxy.
Observations are usually performed using networks of
robotic telescopes.
In addition to the
NASA
/National
Science Foundation-funded OGLE, the Microlensing
Observations in Astrophysics (MOA) group is working to perfect
this approach.
The PLANET (
Probing
Lensing Anomalies NETwork)/RoboNet project is even more
ambitious. It allows nearly continuous round-the-clock coverage by
a world-spanning telescope network, providing the opportunity to
pick up microlensing contributions from planets with masses as low
as Earth. This strategy was successful in detecting the first
low-mass planet on a wide orbit, designated
OGLE-2005-BLG-390Lb.
Circumstellar disks
Disks of space dust (
debris disks)
surround many stars. The dust can be detected because it absorbs
ordinary starlight and re-emits it as
infrared radiation. Even if the dust particles have
a total mass well less than that of Earth, they can still have a
large enough total surface area that they outshine their parent
star in infrared wavelengths.
The
Hubble Space Telescope is
capable of observing dust disks with its NICMOS (Near Infrared
Camera and Multi-Object Spectrometer) instrument. Even better
images have now been taken by its sister instrument, the
Spitzer Space Telescope, which can
see far deeper into
infrared wavelengths
than the Hubble can. Dust disks have now been found around more
than 15% of nearby sunlike stars.
The dust is believed to be generated by collisions among comets and
asteroids. Radiation pressure from the star will push the dust
particles away into interstellar space over a relatively short
timescale. Therefore, the detection of dust indicates continual
replenishment by new collisions, and provides strong indirect
evidence of the presence of small bodies like comets and
asteroids that orbit the parent star. For example,
the dust disk around the star
tau Ceti
indicates that that star has a population of objects analogous to
our own Solar System's
Kuiper Belt, but
at least ten times thicker.
More speculatively, features in dust disks sometimes suggest the
presence of full-sized planets. Some disks have a central cavity,
meaning that they are really ring-shaped. The central cavity may be
caused by a planet "clearing out" the dust inside its orbit. Other
disks contain clumps that may be caused by the gravitational
influence of a planet. Both these kinds of features are present in
the dust disk around
epsilon
Eridani, hinting at the presence of a planet with an orbital
radius of around 40
AU (in
addition to the inner planet detected through the radial-velocity
method).. These kinds of planet-disk interactions can be modeled
numerically using
collisional
grooming techniques.
Contamination of stellar atmospheres
Recent spectral analysis of
white
dwarfs'
atmospheres by
Spitzer Space Telescope
found contamination of heavier elements like
magnesium and
calcium.
These elements cannot originate from the stars' core and it is
probable that the contamination comes from
asteroids got too close (within the
Roche limit) to these stars by gravitational
interaction with larger planets and were torn apart by star's tidal
forces. Spitzer data suggests that 1-3% of the white dwarfs has
similar contamination.
Direct imaging
As mentioned previously, planets are extremely faint light sources
compared to stars and what little light comes from them tends to be
lost in the glare from their parent star. So in general, it is very
difficult to detect them directly. In certain cases, however,
current telescopes may be capable of directly imaging planets.
Projects
to equip the current generation of telescopes with new,
planet-imaging-capable instruments are underway at the Gemini
telescope
(GPI), the
VLT
(SPHERE), and the Subaru
telescope
(HiCiao). Specifically, this may be possible when the planet
is especially large (considerably larger than Jupiter), widely
separated from its parent star, and young (so that it is hot and
emits intense infrared radiation).
In July
2004, a group of astronomers used the European
Southern Observatory
's Very Large Telescope
array in Chile to produce an image of 2M1207b, a companion to the brown dwarf 2M1207. In December 2005, the
planetary status of the companion was confirmed.The planet is
believed to be several times more massive than
Jupiter and to have an orbital radius greater than
40 AU.
The first
multiplanet system, announced on 13 November 2008, was imaged in
2007 using telescopes at both Keck Observatory
and Gemini Observatory
. Three planets were directly observed
orbiting
HR 8799, whose masses are
approximately 10, 10 and 7
times that of
Jupiter. On the same day, 13 November 2008, it was announced
that the Hubble Space Telescope directly observed an exoplanet
orbiting
Fomalhaut with mass no more than
3M
J. Both systems are surrounded by disks not unlike the
Kuiper belt.
Three other possible exoplanets have now been directly imaged:
GQ Lupi b, AB Pictoris b, and SCR 1845 b.
As of March 2006 none have been confirmed as planets; instead, they
might themselves be small
brown
dwarfs.
Future detection methods
Observations from space
Several space missions are planned that will employ already proven
planet-detection methods. Astronomical measurements done from space
can be more sensitive than measurements done from the ground, since
the distorting effect of the Earth's atmosphere is removed, and the
instruments can view in infrared wavelengths that do not penetrate
the atmosphere. Some of these space probes should be capable of
detecting planets similar to our own Earth.
The NASA
Kepler Mission uses the
transit method to scan a hundred
thousand stars in the constellation Cygnus for planets. Kepler will
be sensitive enough to detect planets even smaller than Earth. By
scanning a hundred thousand stars simultaneously, it will not only
be able to detect Earth-sized planets, it will be able to collect
statistics on the numbers of such planets around sunlike
stars.
Kepler has already been able to detect the light from a known
transiting extrasolar gas giant,
HAT-P-7b.
It is expected that Kepler will even be able to detect light from
non-transiting gas giants on close orbits, though it will not be
able to resolve that light into an image. Instead, the brightness
of the host star seems to change gradually over time in a periodic
manner, because like the
Moon, the planet goes
through
phases from full to new and
back again. The variation, although small, will be the signature of
a planet. In addition to the reflected light from the star, some of
the light from the planet will be
thermally emitted by the planet itself.
Thus the shape of the phase curve constrains the composition of the
atmosphere based on the reflectivity of the planet, and also gives
indications of the transport of heat on the planet from the day
side to the night. This planet phase variation method may actually
provide the greatest number of planets to be discovered by the
Kepler satellite, since it does not require the planet to pass in
front of the disk of the star.
NASA's
Space Interferometry
Mission, currently scheduled for launch in 2014, will use
astrometry. It may be able to detect Earth-like planets around
several nearby stars.
The European Space Agency
's Darwin probe and
NASA
's Terrestrial
Planet Finder [362318] probes will attempt to image planets
directly. A recently proposed idea is the
New Worlds Mission, which will use an
occulter to block a star's light, allowing
astronomers to directly observe the dimmer orbiting planets.
(On February 2, 2006 NASA announced an indefinite suspension of
work on the Terrestrial Planet Finder due to budget problems. Then
in June 2006, the Appropriations Committee of the U.S. House of
Representatives partially restored funding, permitting development
work on the project to continue at least through 2007. COROT was
launched on December 27, 2006 and Kepler's launch was performed on
March 7, 2009.)
Huge proposed ground telescopes may also be able to directly image
extrasolar planets. ESO is considering building the
extremely large telescope, with a
mirror diameter between 30 and 60 meters.
Eclipsing binary minima timing
When a
double star system is aligned
such that the stars pass in front of each other in their orbits,
the system is called an "eclipsing binary" star system. The time of
minimum light, when the star with the brighter surface area is at
least partially obscured by the disc of the other star, is called
the primary
eclipse, and approximately half
an orbit later, the secondary eclipse occurs when the brighter
surface area star obscures some portion of the other star. These
times of minimum light, or central eclipse, constitute a time stamp
on the system, much like the pulses from a
pulsar (except that rather than a flash, they are a
dip in the brightness). If there is a planet in circum-binary orbit
around the binary stars, the stars will be offset around a
binary-planet center
of mass. As the stars in the binary are displaced by the planet
back and forth, the times of the eclipse minima will vary; they
will be too late, on time, too early, on time, too late, etc.. The
periodicity of this offset may be the most reliable way to detect
extrasolar planets around close binary systems..
Orbital phase reflected light variations
Short period giant planets in close orbits around their stars will
undergo reflected light variations changes because, like the
Moon, they will go through
phases from full to new and back again.
Although the effect is small — the photometric precision required
is about the same as to detect an Earth-sized planet in transit
across a solar-type star — such Jupiter-sized planets should be
detectable by space telescopes such as the
Kepler Space Observatory. This
method may actually constitute the most planets that will be
discovered by that mission because the reflected light variation
with orbital phase is largely independent of orbital inclination of
the planet's orbit. In addition, the phase function of the giant
planet may be constrained which will, in turn, lead to constraints
on the actual particle size distribution of the atmospheric
particles.
Polarimetry
Light given off by a star is un-polarised, i.e. the direction of
oscillation of the light wave is random. However, when the light is
reflected off the atmosphere of a planet, the light waves interact
with the molecules in the atmosphere and they are polarized.
By analyzing the polarization in the combined light of the planet
and star (about one part in a million), these measurements can in
principle be made with very high sensitivity, as polarimetry is not
limited by the stability of the Earth's atmosphere.
Astronomical devices used for polarimetry, called polarimeters, are
capable of detecting the polarized light and rejecting the
unpolarized beams (starlight). Groups such as ZIMPOL/CHEOPS and
PLANETPOL are currently using polarimeters to search for
extra-solar planets, though no planets have yet been detected using
this method.
See also
References
- "COROT surprises a year after launch", ESA press release 20 December 2007
- ( Preprint at exoplanet.eu)
- Kepler
Mission page
- "Bioastronomy 2002: Life Among the Stars" IAU Symposium 213,
R.P Norris and F.H. Stootman (eds), A.S.P., San Francisco,
California, 80-84.
- Doyle, Laurance R., Hans-Jorg Deeg, J.M. Jenkins, J. Schneider,
Z. Ninkov, R. P.S. Stone, J.E. Blue, H. Götzger, B, Friedman, and
M.F. Doyle (1998). "Detectability of Jupiter-to-brown-dwarf-mass companions
around small eclipsing binary systems". Brown Dwarfs and
Extrasolar Planets, A.S.P. Conference Proceedings, in Brown Dwarfs
and Extrasolar Planets, R. Rebolo, E. L. Martin, and M.R.Z. Osorio
(eds.), A.S.P. Conference Series 134, San Francisco, California,
224-231.
External links