Webb Finds Water in Rare Main-Belt Comet, Spurring New Mysteries

James Webb Space Telescope Comet Read

NASA’s James Webb Space Telescope has helped scientists achieve another breakthrough. Solar system scientists working to understand the origins of Earth’s abundant water have used Webb’s Near-Infrared Spectrograph (NIRSpec) instrument to confirm water vapor around a comet in the main asteroid belt for the first time.

This significant discovery indicates that “water ice from the primordial solar system can be preserved in that region.” The new observations may help reveal where water on Earth came from, answering one of the biggest questions of all: how Earth became host to so much life.

However, like many of Webb’s most interesting and important discoveries, finding water in a main-belt comet has perhaps led to more questions than answers.

“The successful detection of water comes with a new puzzle: unlike other comets, Comet 238P/Read had no detectable carbon dioxide,” NASA explains.

James Webb Space Telescope Comet Read
“This graphic presentation of spectral data highlights a key similarity and difference between observations of Comet 238P/Read by the NIRSpec (Near-Infrared Spectrograph) instrument on NASA’s James Webb Space Telescope in 2022 and observations of Comet 103P/Hartley 2 by NASA’s Deep Impact mission in 2010. Both show a distinct peak in the region of the spectrum associated with water. Finding this in Comet Read was a significant accomplishment for Webb, as it is in a different class of comets than Jupiter-family comets like Hartley 2, and this marks the first time that a gas has been confirmed in such a main belt comet. However, Comet Read did not show the characteristic, expected bump indicating the presence of carbon dioxide.” | Credits: NASA, ESA, CSA, and J. Olmstead (STScI)

“Our water-soaked world, teeming with life and unique in the universe as far as we know, is something of a mystery — we’re not sure how all this water got here. Understanding the history of water distribution in the solar system will help us to understand other planetary systems, and if they could be on their way to hosting an Earth-like planet,” says Stefanie Milam, Webb deputy project scientist for planetary science and co-author of the study reporting the new finding.

The study, “Spectroscopic identification of water emission from a main-belt comet,” has been published in Nature. Additional authors include Michael S. P. Kelley, Henry H. Hsieh, Dennis Bodewits, Mohammad Saki, Geronimo L. Villanueva, and Heidi B. Hammel.

Comet Read (238P) is a main-belt comet, which means that it resides in the solar system’s main asteroid belt but “periodically displays a halo, or coma, and tail like a comet.”

NASA explains that “main belt comets” are a relatively recent classification of celestial objects, and Comet Read was among the three original comets that comprise the first main-belt comets. Before the new category was established, “Comets were understood to reside in the Kuiper Belt and Oort Cloud, beyond the orbit of Neptune, where their ices could be preserved farther from the Sun. Frozen material that vaporizes as they approach the Sun is what gives comets their distinctive coma and streaming tail, differentiating them from asteroids. Scientists have long speculated that water ice could be preserved in the warmer asteroid belt, inside the orbit of Jupiter, but definitive proof was elusive — until Webb.”

The study’s lead author, Michael Kelley of the University of Maryland, explains that only because of precise spectral data from Webb can scientists definitively say that it’s water ice that enables objects in the main belt to show trademark characteristics of comets.

James Webb Space Telescope Comet Read
“This image of Comet 238P/Read was captured by the NIRCam (Near-Infrared Camera) instrument on NASA’s James Webb Space Telescope on September 8, 2022. It displays the hazy halo, called the coma, and tail that are characteristic of comets, as opposed to asteroids. The dusty coma and tail result from the vaporization of ices as the Sun warms the main body of the comet.” | Credits: NASA, ESA, CSA, M. Kelley (University of Maryland). Image processing: H. Hsieh (Planetary Science Institute), A. Pagan (STScI)

“With Webb’s observations of Comet Read, we can now demonstrate that water ice from the early solar system can be preserved in the asteroid belt,” Kelley says.

While the study’s authors are perhaps surprised by the water vapor around Comet Read, the missing carbon dioxide “was a bigger surprise.”

“Typically, carbon dioxide makes up about 10 percent of the volatile material in a comet that can be easily vaporized by the Sun’s heat. The science team presents two possible explanations for the lack of carbon dioxide. One possibility is that Comet Read had carbon dioxide when it formed but has lost that because of warm temperatures,” explains NASA.

Kelley theorizes that because Comet Read has been in the asteroid belt for a long time, carbon dioxide could have evaporated, as carbon dioxide evaporates more quickly than water ice. Kelley also suggests that Comet Read may have formed in an especially warm pocket of the solar system, where there wasn’t any carbon dioxide present. Basically, the two possibilities being considered are that Comet Read had carbon dioxide, but it has since been lost, or it never had carbon dioxide at all because of its environment.

James Webb Space Telescope Comet Read
“This artist’s concept of Comet 238P/Read shows the main belt comet sublimating — its water ice vaporizing as its orbit approaches the Sun. This is significant, as the sublimation is what distinguishes comets from asteroids, creating their distinctive tail and hazy halo, or coma. The James Webb Space Telescope’s detection of water vapor at Comet Read is a major benchmark in the study of main belt comets, and in the broader investigation of the origin of Earth’s abundant water.” | Credits: NASA, ESA

Study co-author Heidi Hammel of the Association of Universities for Research in Astronomy (AURA), and the lead for Webb’s Guaranteed Time Observations for solar system objects, suggests that the next step is to see how other main belt comets compare to Comet Read.

“These objects in the asteroid belt are small and faint, and with Webb we can finally see what is going on with them and draw some conclusions. Do other main belt comets also lack carbon dioxide? Either way it will be exciting to find out,” Hammel says.

“Now that Webb has confirmed there is water preserved as close as the asteroid belt, it would be fascinating to follow up on this discovery with a sample collection mission, and learn what else the main belt comets can tell us,” adds Milam.


Image credits: NASA, ESA, and CSA

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