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When
Do Gas Giants Reach The Point Of No Return?
Thursday, December 6, 2007
The Fine Line Between
Stability And Instability
Gas
Giants
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Credit:
NASA/JPL-Caltech/T. Pyle (SSC)
Planetary scientists at UCL
have identified the point at which a star causes the atmosphere
of an orbiting gas giant to become critically unstable, as
reported in this week’s Nature
(December 6). Depending upon their proximity to a host star,
giant Jupiter-like planets have atmospheres which are either
stable and thin, or unstable and rapidly expanding. This new
research enables us to work out whether planets in other systems
are stable or unstable by using a three dimensional model to
characterize their upper atmospheres.
Tommi Koskinen of UCL’s
Physics & Astronomy Department is lead author of the paper
and says: “We know that Jupiter has a thin, stable
atmosphere and orbits the Sun at five Astronomical Units (AU) -
or five times the distance between the Sun and the Earth. In
contrast, we also know that closely orbiting exoplanets like
HD209458b - which orbits about 100 times closer to its sun than
Jupiter does - has a very expanded atmosphere which is boiling
off into space. Our team wanted to find out at what point this
change takes place, and how it happens.
“Our paper shows that if
you brought Jupiter inside the Earth's orbit, to 0.16AU, it would
remain Jupiter-like, with a stable atmosphere. But if you brought
it just a little bit closer to the Sun, to 0.14AU, its atmosphere
would suddenly start to expand, become unstable and escape. This
dramatic change takes place because the cooling mechanism that we
identified breaks down, leading to the atmosphere around the
planet heating up uncontrollably.”
Professor Alan Aylward,
co-author of the paper, explains some of the factors which the
team incorporated in order to make the breakthrough: “For
the first time we’ve used 3D-modeling to help us understand
the whole heating process which takes place as you move a gas
giant closer to its sun. The model incorporates the cooling
effect of winds blowing around the planet - not just those
blowing off the surface and escaping.
“Crucially, the model
also makes proper allowances for the effects of H3+ in
the atmosphere of a planet. This is an electrically-charged form
of hydrogen which strongly radiates sunlight back into space and
which is created in increasing quantities as you heat a planet by
bringing it closer to its star.
“We found that 0.15AU is
the significant point of no return. If you take a planet even
slightly beyond this, molecular hydrogen becomes unstable and no
more H3+ is produced. The self-regulating,
‘thermostatic’ effect then disintegrates and the
atmosphere begins to heat up uncontrollably.”
Professor Steve Miller, the
final contributing author to the paper, puts the discovery into
context: “This gives us an insight to the evolution of
giant planets, which typically form as an ice core out in the
cold depths of space before migrating in towards their host star
over a period of several million years. Now we know that at some
point they all probably cross this point of no return and undergo
a catastrophic breakdown.
“Just twelve years ago
astronomers were searching for evidence of the first extrasolar
planet. It’s amazing to think that since then we’ve
not only found more than 250 of them, but we’re also in a
much better position to understand where they came from and what
happens to them during their lifetime.”
Source:
University College London

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