{"id":646,"date":"2024-05-21T08:22:31","date_gmt":"2024-05-21T08:22:31","guid":{"rendered":"https:\/\/isog.xyz\/?p=646"},"modified":"2024-05-21T08:22:31","modified_gmt":"2024-05-21T08:22:31","slug":"webb-space-telescope-cracks-case-of-puffy-microwaved-marshmallow-exoplanet","status":"publish","type":"post","link":"https:\/\/isog.xyz\/?p=646","title":{"rendered":"Webb Space Telescope Cracks Case of Swollen Exoplanet “Microwave Marshmallow”."},"content":{"rendered":"
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\"Neptune<\/p>\n

The warm gas giant WASP-107 b, known for its unusually low density and moderate temperature, may have an inflated atmosphere due to tidal heating that warms its interior more than previously thought. (Artist’s concept.) Credit: SciTechDaily.com<\/p>\n<\/div>\n

A surprising depletion of methane suggests that tidal heating has puffed up the atmosphere of warm gas giant WASP-107 b.<\/h3>\n

Why is the warm gas giant exoplanet<\/span> WASP-107 b so, so swollen? With a moderate temperature and an ultra-low density comparable to that of a microwaved marshmallow, it appears to defy standard theories of planet formation and evolution.<\/em><\/p>\n

Two independent teams of researchers think they have figured it out. Data from Webb, combined with previous observations from Hubble, show that WASP-107 b’s interior must be much toastier than previously estimated. The unexpectedly high temperature, thought to be caused by tidal forces that stretch the planet like dumb putty, could explain how planets like WASP-107 b can be so floating, potentially solving a long-standing mystery in exoplanet science.<\/em><\/p>\n

\"Warm<\/p>\n

This artist’s concept shows what the exoplanet WASP-107 b might look like based on recent data collected by NASA’s James Webb Space Telescope, along with previous observations from Hubble and other space-based and ground-based telescopes. WASP-107 b is a ‘warm Neptune’ exoplanet orbiting a relatively small and cool star, about 210 light-years from Earth, in the constellation Virgo. The planet is about 80% the size of Jupiter by volume, but has a mass less than 10% of Jupiter, making it one of the least dense exoplanets known. Credit: NASA, ESA, CSA, Ralf Crawford (STScI)<\/p>\n<\/div>\n

Webb space telescope cracks case of blown-up exoplanet<\/h3>\n

Why is the warm gas giant exoplanet WASP-107 b so swollen? Two independent research teams now have an answer.<\/p>\n

Data collected using NASA’s James Webb Space Telescope, combined with previous observations from NASA’s Hubble Space Telescope, show surprisingly little methane (CH4<\/sub>) in the planet’s atmosphere. This indicates that WASP-107 b’s interior must be significantly hotter and its core much more massive than previously estimated.<\/p>\n

The unexpectedly high temperature is thought to be the result of tidal heating caused by the planet’s slightly non-circular orbit, and may explain how WASP-107 b could have become so blown up without resorting to extreme theories about how it formed.<\/p>\n

The results, made possible by Webb’s extraordinary sensitivity and associated ability to measure light passing through the atmospheres of exoplanets, could explain the walls of dozens of low-density exoplanets and help solve a long-standing mystery in exoplanet science .<\/p>\n

The problem with WASP-107 b<\/h4>\n

At more than three-quarters of the volume of Jupiter<\/span> but less than a tenth of the mass, the ‘warm’ Neptune<\/span>exoplanet WASP-107 b is one of the least dense planets known. Although puffy planets are not uncommon, most are hotter and more massive, and therefore easier to explain.<\/p>\n

\u201cBased on its radius, mass, age and presumed internal temperature, we thought WASP-107 b had a very small, rocky core surrounded by a huge mass of hydrogen and helium,\u201d explains Luis Welbanks of Arizona State University (ASU). out. lead author of a paper published in the journal on May 20 Nature<\/em>. ‘But it was difficult to understand how such a small core could suck in so much gas and then not fully develop into a planet with the mass of Jupiter.’<\/p>\n

\"Warm<\/p>\n

This transmission spectrum, captured using NASA’s Hubble and James Webb space telescopes, shows the amounts of different wavelengths (colors) of starlight blocked by the atmosphere of the gas giant exoplanet WASP-107 b.
The spectrum includes light collected over five separate observations using a total of three different instruments: Hubble’s WFC3 (0.8\u20131.6 microns), Webb’s NIRCam (2.4\u20134.0 microns and 3.9\u20135 .0 microns) and Webb’s MIRI (5\u201312 microns). Each set of measurements was made by observing the planet-star system for about ten hours before, during and after the transit as the planet moved along the star’s surface.
By comparing the brightness of light filtered through the planet’s atmosphere (transmitted light) with unfiltered starlight, it is possible to calculate the amount of each wavelength blocked by the atmosphere. Because each molecule absorbs a unique combination of wavelengths, the transmission spectrum can be used to limit the abundance of different gases.
This spectrum shows clear evidence for water (H2O), carbon dioxide (CO2), carbon monoxide (CO), methane (CH4), sulfur dioxide (SO2) and ammonia (NH3) in the planet’s atmosphere, allowing researchers to examine the planet’s interior to estimate. temperature and mass of the core.
This wavelength coverage from optical to mid-infrared is the broadest transmission spectrum of any exoplanet to date, and includes the first reported detection by space telescopes of ammonia in an exoplanet’s atmosphere.
Credit: NASA, ESA, CSA, Ralf Crawford (STScI), Luis Welbanks (ASU), JWST MANATEE Team<\/p>\n<\/div>\n

If WASP-107 b instead had more of its mass in its core, its atmosphere should have contracted as the planet cooled over time since its formation. Without a heat source to re-expand the gas, the planet would be much smaller. Although WASP-107 b has an orbital distance of only 8 million kilometers (one-seventh the distance between Mercury and the Sun), it does not receive enough energy from its star to become so blown up.<\/p>\n

“WASP-107 b is such an interesting target for Webb because it is significantly cooler and more Neptune-like in mass than many of the other low-density planets, the hot Jupiters, that we have studied,” says David Sing of the Johns. Hopkins University (JHU), lead author of a parallel study also published today in Nature<\/em>. \u201cAs a result, we should be able to detect methane and other molecules that could give us information about its chemistry and internal dynamics that we can’t get from a hotter planet.\u201d<\/p>\n

A wealth of previously undetectable molecules<\/h4>\n

WASP-107 b’s massive radius, extensive atmosphere and peripheral orbit make it ideal for transmission spectroscopy, a method used to identify the different gases in an exoplanet’s atmosphere based on how they affect starlight.<\/p>\n

By combining observations from Webb’s NIRCam (Near-Infrared Camera), Webb’s MIRI (Mid-Infrared Instrument) and Hubble’s WFC3 (Wide Field Camera 3), Welbanks’ team was able to capture a broad spectrum from 0.8 to 12.2 microns absorbed building up light through the atmosphere of WASP-107 b. Using Webb’s NIRSpec (Near-Infrared Spectrograph), Sing’s team built an independent spectrum from 2.7 to 5.2 microns.<\/p>\n

The accuracy of the data makes it possible to determine not only the abundance of molecules, including water vapor (H2<\/sub>O), methane (CH4<\/sub>), carbon dioxide (CO2<\/sub>), carbon monoxide (CO), sulfur dioxide (SO2<\/sub>) and ammonia (NH3<\/sub>).<\/p>\n

\"Warm<\/p>\n

This transmission spectrum, recorded using Webb’s NIRSpec (Near-Infrared Spectrograph), shows the amounts of different wavelengths (colors) of near-infrared starlight blocked by the atmosphere of the gas giant exoplanet WASP-107 b.
The spectrum was created by observing the planet-star system for about 8.5 hours before, during and after the transit as the planet moved along the star’s surface.
By comparing the brightness of light filtered through the planet’s atmosphere (transmitted light) with unfiltered starlight, it is possible to calculate the amount of each wavelength blocked by the atmosphere. Because each molecule absorbs a unique combination of wavelengths, the transmission spectrum can be used to limit the abundance of different gases.
This spectrum shows clear evidence for water (H2O), carbon dioxide (CO2), carbon monoxide (CO), methane (CH4) and sulfur dioxide (SO2) in the planet’s atmosphere, allowing researchers to estimate the interior temperature and mass of the atmosphere. core.
Credits: NASA, ESA, CSA, Ralf Crawford (STScI), David Sing (JHU), NIRSpec GTO Transiting Exoplanet Team<\/p>\n<\/div>\n

Boiling gas, hot interior and huge core<\/h4>\n

Both spectra show a surprising lack of methane in WASP-107 b’s atmosphere: one thousandth of the expected amount based on the assumed temperature.<\/p>\n

\u201cThis is evidence that hot gas from deep within the planet must mix vigorously with the cooler layers higher up,\u201d Sing explains. \u201cMethane is unstable at high temperatures. The fact that we detected so little, even though we did detect other carbonaceous molecules, tells us that the interior of the planet must be significantly hotter than we thought.\u201d<\/p>\n

A likely source of WASP-107 b’s extra internal energy is tidal heating, caused by its somewhat elliptical orbit. As the distance between the star and the planet continually changes during its 5.7-day orbit, the force of gravity also changes, stretching and heating the planet.<\/p>\n

Researchers had previously proposed that tidal heating could be the cause of WASP-107 b’s ramparts, but until the Webb results came in, there was no evidence.<\/p>\n

Once they determined that the planet has enough internal heat to thoroughly shake up its atmosphere, the teams realized that the spectra could also provide a new way to estimate the size of the core.<\/p>\n

\u201cIf we know how much energy is on the planet, and we know what part of the planet is made up of heavier elements like carbon, nitrogen, oxygen and sulfur, versus how much hydrogen and helium, we can calculate how much mass it must contain. the core,\u201d explains Daniel Thorngren of JHU.<\/p>\n

It turns out that the core is at least twice as massive as originally estimated, which makes more sense in terms of how planets form.<\/p>\n

All in all, WASP-107 b is not as mysterious as it once seemed.<\/p>\n

\u201cThe Webb data tells us that planets like WASP-107 b didn’t have to form in some strange way with a super small core and a huge gaseous envelope,\u201d explains ASU’s Mike Line. “Instead, we can take something that looks more like Neptune, with a lot of rock and not so much gas, just raise the temperature and crank it up to look like this.”<\/p>\n

Reference: \u201cA high internal heat flux and large core in a warm Neptune exoplanet\u201d by Luis Welbanks, Taylor J. Bell, Thomas G. Beatty, Michael R. Line, Kazumasa Ohno, Jonathan J. Fortney, Everett Schlawin, Thomas P. Greene, Emily Rauscher, Peter McGill, Matthew Murphy, Vivien Parmentier, Yao Tang, Isaac Edelman, Sagnick Mukherjee, Lindsey S. Wiser, Pierre-Olivier Lagage, Achr\u00e8ne Dyrek and Kenneth E. Arnold, May 20, 2024, Nature<\/i>.
DOI: 10.1038\/s41586-024-07514-w<\/p>\n

The James Webb Space Telescope<\/span> is the world’s premier space science observatory. Webb solves mysteries in our solar system, looks beyond to distant worlds around other stars and investigates the mysterious structures and origins of our universe and our place in it. Webb is an international program led by NASA<\/span> with its partners, ESA (European Space Agency<\/span>) and CSA (Canadian Space Agency).<\/em><\/p>\n<\/div>\n