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By Mike Brown, Al Conrad, and Linda Copman
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| Image: The old solar system, traditional nine-planet model
of the solar system. Image by Mike Brown, Caltech. |
“It seemed clear to me that no one had ever
really looked hard for large objects that might be distant
and that there was a good chance that they would be out
there. I started to do the first large-scale survey of
the outer solar system since Clyde Tombaugh found Pluto
in 1930. Since 1998, we have surveyed about 50 percent of the
sky.” — Mike Brown
For the past eight years the adaptive optics (AO) system at
Keck Observatory has provided fabulous opportunities to observe
objects that are relatively bright. This includes most bodies
in our solar system, which are well lit by the Sun. But as
you move farther from the center of the solar system, you reach
the point at which sunlight reflected off even small bodies
is too faint to allow “locking the loops” of the Keck AO system.
The Kuiper Belt Objects (KBOs) are, in fact, that distant.
The KBOs that orbit the Sun at the distance of Pluto and beyond
do not reflect enough sunlight to enable a traditional AO system
to “lock” and correct for the blurring effects of the Earth’s
atmosphere.
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| Image: Artist’s conception of the view
from Eris with its moon Dysnomia in the background, looking
back towards the distant sun. Eris was discovered using
the Samuel
Oschin Telescope, a smaller, robotic telescope at
Mt. Palomar. Credit: Robert Hurt, IPAC. |
Then, about two years ago, Keck Observatory pioneered its laser
guide star adaptive optics (LGS AO) system, enabling astronomers
to utilize the AO system while it was pointed at faint objects.
This is done by using a laser to create a bright beacon at
the top of the Earth’s atmosphere and locking the AO system
on that brighter beacon, instead of on the faint target of
scientific interest. Mike Brown, an astronomer at the California
Institute of Technology, used the laser AO system at Keck Observatory
to track the orbit of a small moon orbiting around the KBO
named Eris. Eris is the larger-than-Pluto KBO that started
the great planet debate.
The large telescope mirror at Keck Observatory, along with
AO, are needed to follow up the discovery of KBOs with detailed
studies to determine their composition, for example, or to
look for moons. Brown discovered a moon of Eris using the NIRC2
instrument and adaptive optics with the Keck II Telescope.
By following the orbit of this moon, named Dysnomia, Brown
was able to estimate the mass of Eris.
Several observations of the orbit were taken with both the
Hubble Space Telescope and the Keck II Telescope.
“As soon as we find these objects, the first
thing we always want to do is to get out to Keck to look
at the spectrum of sunlight reflected from their surface
to try to determine what they are made of. For the very
largest objects, we can use the laser guide star adaptive
optics system to see if they have satellites. This approach
has been >very< fruitful.” — Mike Brown
So what makes Mercury, Venus, Earth, Mars, Jupiter, Saturn,
Uranus, and Neptune planets, and Pluto and Eris not planets?
The short answer to this question is provided by the International
Astronomical Union (IAU) resolution, which was passed by a
vote of 237 to 157 on August 24, 2006, and reads as follows:
“The IAU...resolves that planets and other
bodies, except satellites, in our Solar System be defined
into three distinct categories in the following way:
(1) A planet is a celestial body that (a) is in orbit around
the Sun, (b) has sufficient mass for its self-gravity to
overcome rigid body forces so that it assumes a hydrostatic
equilibrium (nearly round) shape, and (c) has cleared the
neighbourhood around its orbit.
(2) A ‘dwarf planet’ is a celestial body that (a) is in orbit
around the Sun, (b) has sufficient mass for its self-gravity
to overcome rigid body forces so that it assumes a hydrostatic
equilibrium (nearly round) shape, (c) has not cleared the
neighbourhood around its orbit, and (d) is not a satellite.
(3) All other objects, except satellites, orbiting the Sun
shall be referred to collectively as ‘Small Solar System
Bodies.’”
What this means is that a planet must orbit the Sun by itself,
and not just be hitch-hiking as a moon in orbit around some
another body, and must be “big enough.” It is this “big enough” question
that results in a gray area - and seems to get people’s dander
up.
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| Image: The orbits of a number of main belt
asteroids (in brown) plotted together with major
planet orbits (in blue). Image by Celestia,
copyright (C) 2001-2005, Chris Laurel. |
Early in their week-long meeting in Prague last year, IAU members
thought they had hit upon a big-ness criteria that really captured “planet-ness.” The
very small bodies in the solar system tend to be shaped like
sea otters, potatoes, tennis shoes, dog bones, and other household
items, but generally, they are not the nice, spherical shapes
we associate with planets. This is because a solar system body
must have a certain mass before its own gravity will overcome
the internal, rigid forces that strive to retain whatever oddball
shape resulted from the formation process. The effectiveness
of the gravitational forces trying to make the body relax into
a spherical shape, and the rigid forces resisting that process,
both depend on things like density and composition, which vary
from body to body. So it is not possible to simply specify
a diameter, like say 1000 kilometers, above which a body is
round and therefore a planet.
However, it turns out that on average, the right diameter is
about 1000 km. As an example, of all of the million or so bodies
floating in the asteroid belt between Mars and Jupiter, only
one is round. This is Ceres, which is about 1000 km in diameter.
All of the other million-minus-one asteroids in the belt are
smaller than about 700 km and have oddball shapes.
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Image: Taking the number of planets from
9 to 53 dramatically changes the look of the solar system.
Here is a picture showing the old planets (black
circles) and potential new planets (add red
ellipses). Image and caption by Mike Brown, Caltech.
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Early on in the meeting, the IAU had a simple definition for
a planet: it must orbit the Sun and be round. The new body,
Eris, satisfied both criteria, so it would become the 10th
planet. Ceres meets both criteria, too, so that’s 11 planets.
There’s also Charon (Pluto’s neighbor), so that makes 12. There
were getting to be a lot of potential planets.
But where would that lead us? Many planetary scientists believe
that, following future discoveries, Eris will be joined by
many other large, round bodies. Eris is part of another large “neighborhood” in
our solar system called the Kuiper Belt, which is like the
asteroid belt but further away and colder. So we could potentially
end up with 50, or even 100, “planets.”
This is the point, mid-week of the IAU meeting, at which the
debate really started heating up. In the end, the IAU resolved
the problem by adding a clause to the definition, stating that
a planet “has cleared the neighbourhood around its orbit.” This
new clause takes care of the potential 50 to 100 yet-to-be-discovered
Kuiper Belt objects; it takes care of Eris, Ceres, and Charon;
and it also takes care of Pluto.
“Planets are the large dominant objects in
the solar system. If you removed a planet, everything else
would have to adjust to make up for the loss. Dwarf planets
look like planets in that they’re round, but there are
hundreds of them and no one would notice if you took away
a few or added a few. There are millions and millions of
other bodies (no one quite knows what the official term
is these days….) that are so small as to not be round.” — Mike
Brown
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| Image: Planets from the first and second
(final) IAU resolutions. Courtesy of NASA/JPL-Caltech,
with caption and edits in red by Al Conrad, Keck Support
Astronomer. |
Click
here for a video clip of one possible scenario for the
evolution of our solar system (requires Quicktime player).
The movie begins with the giant planets (Jupiter through Neptune)
in circular orbits around the sun, with a dense belt of icy
objects beyond (in green). As millions of years (Myr) pass,
gaps appear in the proto-Kuiper Belt. The premise of this animation
is that over the course of a billion years, continual gravitational
encounters with small solar system bodies gradually altered
the orbits of the outer planets. Learn
more here.
Why has the recognition that Pluto is not really a planet resulted
in such a cosmic shake-up? There are several reasons. First,
the fact that the IAU itself did not reach a clear-cut consensus
on the definition of a planet until the end of the meeting
left many people confused. Second, some folks wonder whether
the scientific community should even be messing with the more
romantic notion of a planet. Third, there are now a tremendous
number of text books, posters, wall maps, 3-D models, encyclopedias,
and dictionaries that have to be revised. Educators are in
a tough position.
Or maybe this is precisely what science is all about. West
Hawai`i District Superintendent for the Department of Education,
Art Souza, sees the demotion of Pluto as an opportunity to
make science meaningful to young people:
“I wonder if Pluto becomes just a note in a
textbook ‘correcting an error,’ or if it can it be the
basis of deep and reflective conversations in classrooms
across America? Pluto gives us an opportunity. Can we make
this a larger moment, a teachable moment that allows kids
to ‘think about’ the consequences of this decision in the
framework of larger implications for research and scientific
knowledge? Is it so important that Pluto has been downgraded?
How is this relevant and how does it impact long held ‘knowledge-based
beliefs’? How is this important in terms of what kids need
to know about the universe and their role in it?” -
Art Souza
Quite a few astronomers and members of the public agree with
Souza that the shake-up is good. Al Conrad, support astronomer
at Keck Observatory, shares these thoughts: “The general population
should not be hung up on a pigeon-hole definition, but should
be more interested in our ever-changing understanding of the
cosmos,” says Conrad.
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| Photo: Mike Brown and Emily Schaller working
at Keck Observatory. Photo courtesy of Emily Schaller,
August 30, 2006. |
There exists a striking parallel between what happened with
Pluto between 1930 and 2006, and what happened with Ceres between
1801 and 1850. Both were discovered and quickly identified
as planets (in 1801 and 1930, respectively). They were later
reclassified as non-planets about half a century later (in
1850 and 2006, respectively) because they were determined to
be part of a larger, nearby population. Pluto, in the distant
Kuiper Belt, just took about two hundred years longer to explore
than Ceres did, because we needed larger telescopes, like those
at Keck Observatory to do it. “This historical perspective
of looking at what happened with Ceres goes a long way toward
supporting the resolution passed by the IAU and validating
where we stand today with the definition of a planet,” suggests
Conrad.
One of Brown’s graduate students, Emily Schaller, has had the
privilege of observing at Keck Observatory with her mentor
roughly 55 times, “which is more than many astronomers could
ever hope for in their lifetimes,” she says. Schaller is thrilled
to be working on the cutting edge of planetary astronomy so
early in her career. One particular evening stands out in her
mind:
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| Photo: Mike Brown sporting 3-D glasses. |
“In my third year of graduate school, after I had been coming
to Keck for a while with Mike to observe objects in the outer
solar system, I had the opportunity to be in charge of an observing
run while Mike stayed home in preparation for the birth of
his daughter. Late that night, Kris Barkume (another graduate
student in our group) and I swung the Keck I Telescope around
to look at a newly discovered dwarf planet around which our
group had just discovered a moon using Keck LGS AO. Much to
our surprise, we actually saw the moon with NIRC (under extremely
good conditions), and, even though it was not what I was supposed
to be doing, I decided that the best use of the time was to
target the tiny moon itself to see what it was made of. When
I called Mike the next day to tell him, he sounded grumpy,
as if we had perhaps been wasting our time on something that
was impossible, but within a few hours he called back and let
us know that, in fact, our observations showed something remarkable:
the satellite of the dwarf planet was unlike anything that
had ever been observed in the solar system before. We now know
that the moon formed when two dwarf planets collided at high
speed, leaving one dwarf planet and a tiny moon. Knowing that
I made a decision that led to this discovery is a great feeling.” — Emily
Schaller, doctoral candidate at Caltech
To listen to Mike Brown’s lecture and view his Powerpoint presentation
on “Pluto and Other Dwarf Planets: Discoveries in Our Solar
System” visit Keck Observatory's Podcast page. 
Click here to return to the main
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