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comet_K2

Comet or Nibiru? Hubble Spots Supposed ‘Comet K2’ – Farthest Active INBOUND Comet To Date

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This initially seemed like an ordinary article in regards to it’s subject, though very interesting in the contents but it is far more interesting than I initially thought.

There is something troubling with some of the facts presented in this article, namely why there is a coma around a comet at such an incredibly vast distance. Normally the sun would cause comets to form their coma (evaporation of water ice) but these would be much closer to the sun. The researcher claims instead that this comet’s coma is likely being caused by sublimation [a solid changing directly into a gas]…one problem there,

he says, “…Slightly warmed by the remote Sun…”

but according the Wikipedia, the surface temperature of Saturnian moon Titan is −179.5 °C. Titan is over half a billion miles closer to the Sun than is this comet. Note also that the article mentions the comet is in the frigid outer reaches of the solar system, where the temperature is about minus 440 degrees Fahrenheit!

So given that extreme cold and massively vast distance, are we supposed to believe that the “warmth” of the Sun is causing this comet to sublimate? REALLY?

via Phys.org:

NASA’s has photographed the farthest active inbound comet ever seen, at a whopping distance of 1.5 billion miles from the Sun (beyond Saturn’s orbit). Slightly warmed by the remote Sun, it has already begun to develop an 80,000-mile-wide fuzzy cloud of dust, called a coma, enveloping a tiny, solid nucleus of frozen gas and dust. These observations represent the earliest signs of activity ever seen from a comet entering the solar system’s planetary zone for the first time.

The comet, called C/2017 K2 (PANSTARRS) or “K2”, has been travelling for millions of years from its home in the frigid outer reaches of the solar system, where the temperature is about minus 440 degrees Fahrenheit. The comet’s orbit indicates that it came from the Oort Cloud, a spherical region almost a light-year in diameter and thought to contain hundreds of billions of comets. Comets are the icy leftovers from the formation of the solar system 4.6 billion years ago and therefore pristine in icy composition.

“K2 is so far from the Sun and so cold, we know for sure that the activity-all the fuzzy stuff making it look like a comet-is not produced, as in other comets, by the evaporation of water ice,” said lead researcher David Jewitt of the University of California, Los Angeles. “Instead, we think the activity is due to the sublimation [a solid changing directly into a gas] of super-volatiles as K2 makes its maiden entry into the solar system’s planetary zone. That’s why it’s special. This comet is so far away and so incredibly cold that water ice there is frozen like a rock.”

Based on the Hubble observations of K2’s coma, Jewitt suggests that sunlight is heating frozen volatile gases – such as oxygen, nitrogen, carbon dioxide, and carbon monoxide – that coat the comet’s frigid surface. These icy volatiles lift off from the comet and release dust, forming the coma. Past studies of the composition of comets near the Sun have revealed the same mixture of volatile ices.

“I think these volatiles are spread all through K2, and in the beginning billions of years ago, they were probably all through every comet presently in the Oort Cloud,” Jewitt said. “But the volatiles on the surface are the ones that absorb the heat from the Sun, so, in a sense, the comet is shedding its outer skin. Most comets are discovered much closer to the Sun, near Jupiter’s orbit, so by the time we see them, these surface volatiles have already been baked off. That’s why I think K2 is the most primitive comet we’ve seen.”

K2 was discovered in May 2017 by the Panoramic Survey Telescope and Rapid Response System (Pan-STARRS) in Hawaii, a survey project of NASA’s Near-Earth Object Observations Program. Jewitt used Hubble’s Wide Field Camera 3 at the end of June to take a closer look at the icy visitor.

Hubble’s sharp “eye” revealed the extent of the coma and also helped Jewitt estimate the size of the nucleus-less than 12 miles across-though the tenuous coma is 10 Earth diameters across.

This vast coma must have formed when the comet was even farther away from the Sun. Digging through archival images, Jewitt’s team uncovered views of K2 and its fuzzy coma taken in 2013 by the Canada-France-Hawaii Telescope (CFHT) in Hawaii. But the object was then so faint that no one noticed it.

“We think the comet has been continuously active for at least four years,” Jewitt said. “In the CFHT data, K2 had a coma already at 2 billion miles from the Sun, when it was between the orbits of Uranus and Neptune. It was already active, and I think it has been continuously active coming in. As it approaches the Sun, it’s getting warmer and warmer, and the activity is ramping up.”

But, curiously, the Hubble images do not show a tail flowing from K2, which is a signature of comets. The absence of such a feature indicates that particles lifting off the comet are too large for radiation pressure from the Sun to sweep them back into a tail.

Astronomers will have plenty of time to conduct detailed studies of K2. For the next five years, the comet will continue its journey into the inner solar system before it reaches its closest approach to the Sun in 2022 just beyond Mars’ orbit. “We will be able to monitor for the first time the developing activity of a comet falling in from the Oort Cloud over an extraordinary range of distances,” Jewitt said. “It should become more and more active as it nears the Sun and presumably will form a tail.”

Jewitt said that NASA’s James Webb Space Telescope, an infrared observatory scheduled to launch in 2018, could measure the heat from the nucleus, which would give astronomers a more accurate estimate of its size.

The team’s results will appear in the September 28 issue of The Astrophysical Journal Letters.

More information: David Jewitt et al. A Comet Active Beyond the Crystallization Zone, The Astrophysical Journal (2017). DOI

Journal reference: Astrophysical Journal Letters

Provided by: NASA

Phys.org

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