“Jupiter CSI”: 2009 Impact Scar Big as the Pacific Caused By Titanic-Sized Asteroid

  Jupiter-Impact-Scar

A hurtling asteroid about the size of the Titanic caused the scar that appeared in
Jupiter's atmosphere on July 19, 2009, according to Glenn Orton, an astronomer at NASA's Jet Propulsion Laboratory and Leigh Fletcher, researcher at Oxford University,
U.K.


Data from three infrared telescopes enabled scientists to observe the warm
atmospheric temperatures and unique chemical conditions associated with the
impact debris.  By piecing together signatures of the gases and dark debris
produced by the impact shockwaves, an international team of scientists was able to
deduce that the object was more likely a rocky asteroid than an icy comet.

“Both the fact that the impact itself happened at all and the implication that it may
well have been an asteroid rather than a comet shows us that the outer solar
system is a complex, violent and dynamic place, and that many surprises may be
out there waiting for us,” said Orton. “There is still a lot to sort out in the outer
solar system.”

The new conclusion is also consistent with evidence from results from NASA's
Hubble Space Telescope indicating the impact debris in 2009 was heavier or
denser than debris from comet Shoemaker-Levy 9, the last known object to hurl
itself into Jupiter’s atmosphere in 1994.

Before this collision, scientists had thought that the only objects that hit Jupiter
were icy comets whose unstable orbits took them close enough to Jupiter to be
sucked in by the giant planet's gravitational attraction. Those comets are known as
Jupiter-family comets. Scientists thought Jupiter had already cleared most other
objects, such as asteroids, from its sphere of influence. Besides Shoemaker-Levy,
scientists know of only two other impacts in the summer of 2010, which lit up
Jupiter's atmosphere.

The July 19, 2009 object likely hit Jupiter between 9 a.m. and 11 a.m. UTC. Amateur
astronomer Anthony Wesley from Australia was the first to notice the scar on
Jupiter, which appeared as a dark spot in visible wavelengths.  The scar appeared
at mid-southern latitudes.  Wesley tipped off Orton and colleagues, who
immediately used existing observing time at NASA's Infrared Telescope Facility in
Mauna Kea, Hawaii, the following night and proposed observing time on a host of
other ground-based observatories. Data were acquired at regular
intervals during the week following the 2009 collision.

The data showed that the impact had warmed Jupiter's lower stratosphere by as
much as 3 to 4 Kelvin at about 42 kilometers above its cloudtops. Although 3 to 4
Kelvin does not sound like a lot, it is a significant deposition of energy because it is
spread over such an enormous area.

Plunging through Jupiter’s atmosphere, the object created a channel of super-
heated atmospheric gases and debris.  An explosion deep below the clouds –
probably releasing at least around 200 trillion trillion ergs of energy, or more than
5 gigatons of TNT — then launched debris material back along the channel, above
the cloud tops, to splash back down into the atmosphere, creating the aerosol
particulates and warm temperatures observed in the infrared. The blowback
dredged up ammonia gas and other gases from a lower part of the atmosphere
known as the troposphere into a higher part of the atmosphere known as the
stratosphere.

"Comparisons between the 2009 images and the Shoemaker-Levy 9 results are
beginning to show intriguing differences between the kinds of objects that hit
Jupiter," Fletcher said. "The dark debris, the heated atmosphere and upwelling of
ammonia were similar for this impact and Shoemaker-Levy, but the debris plume in
this case didn’t reach such high altitudes, didn’t heat the high stratosphere, and
contained signatures for hydrocarbons, silicates and silicas that weren’t seen
before. The presence of hydrocarbons, and the absence of carbon monoxide,
provide strong evidence for a water-depleted impactor in 2009."

The detection of silica in this mixture of Jovian atmospheric gases, processed bits
from the impactor and byproducts of high-energy chemical reactions was
significant because abundant silica could only be produced in the impact itself, by a
strong rocky body capable of penetrating very deeply into the Jovian atmosphere
before exploding, but not by a much weaker comet nucleus. Assuming that the
impactor had a rock-like density of around 2.5 grams per cubic centimeter (160
pounds per cubic foot), scientists calculated a likely diameter of 200 to 500 meters
(700 to 1,600 feet).

Scientists computed the set of possible orbits that would bring an object into
Jupiter in the right range of times and at the right locations. Then they searched the
catalog of known asteroids and comets to find the kinds of objects in these orbits.
An object named 2005 TS100 – which is probably an asteroid but could be an
extinct comet – was one of the closest matches. Although this object was not the
actual impactor, it has a very chaotic orbit and made several very close approaches
to Jupiter in computer models, demonstrating that an asteroid could have hurtled
into Jupiter.

"We weren't expecting to find that an asteroid was the likely culprit in this impact,
but we've now learned Jupiter is getting hit by a diversity of objects," said Paul
Chodas, a scientist at NASA's Near-Earth Object Program Office at JPL. " Asteroid
impacts on Jupiter were thought to be quite rare compared to impacts from the so-
called 'Jupiter-family comets,' but now it seems there may be a significant
population of asteroids in this category."

Scientists are still working to figure out what that frequency at Jupiter is, but
asteroids of this size hit Earth about once every 100,000 years.  The next steps in
this investigation will be to use detailed simulations of the impact to refine the size
and properties of the impactor, and to continue to use imaging at infrared, as well
as visible wavelengths, to search for debris from future impacts of this size or
smaller.

The infrared image below showing thermal radiation at a wavelength of 9.7 microns, was obtained by the Gemini North Telescope in Hawaii. The image shows the aftermath of an impactor hitting Jupiter on July 19, 2009. The area of impact can be seen as the bright white and yellow features at the bottom of this image. An inset shows the impact area in more detail. The image was taken on July 22, 2009, three days after the impact. White and yellow indicate hot temperatures and the presence of hot ammonia upwelling from deep in Jupiter's atmosphere. Infrared images like this, along with measurements of light intensity at different wavelengths to look for the unique signatures of different materials that were obtained by the Gemini South Telescope in Chile, strongly suggest to scientists that a rocky body slammed into the Jovian atmosphere. That body was likely an asteroid and not a comet.

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The Daily Galaxy via jpl.nasa

Image credit: Gemini Observatory/AURA/UC Berkeley/SSI/ JPL-Caltech

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