Showing posts with label exoplanetary systems. Show all posts
Showing posts with label exoplanetary systems. Show all posts

Monday, December 06, 2021

Giant planets could reach “maturity” much earlier than previously thought

Credit: Gabriel Pérez Díaz, SMM (IAC)

Credit: Gabriel Pérez Díaz, SMM (IAC)

An international team of scientists has successfully measured the masses of the giant planets of the V1298 Tau system, which is just 20 million years old. For this result they have used radial velocity measurements from telescopes on La Palma, in southern Spain and on Tenerife, including the STELLA II telescope from the Leibniz Institute for Astrophysics Potsdam (AIP). Masses for such young giant planets had not been obtained previously. The study now published in Nature Astronomy delivers the first evidence that these objects can reach their final size within their first millions of years of evolution.

The study reports the measurement of the masses of two giant planets that orbit the young solar-type star V1298 Tau,whose total lifetime is about 10 billion years. They were discovered in 2019 using data from NASA's Kepler space telescope, which allowed the measurement of their sizes, slightly smaller than Jupiter, and of their orbital periods, 24 and 40 days for V1298 Tau b and e, respectively.

“The characterization of very young planets is extraordinarily difficult,” says the first author of the study Dr Alejandro Suárez Mascareño from the Instituto de Astrofísica de Canarias (IAC). “The parent stars have very high levels of activity and until very recently it was unthinkable to even try”. He adds: “Only thanks to detections made with space telescopes, combined with intense radial velocity campaigns from Earth-based observatories and the use of the most advanced analysis techniques, it was possible to begin to see what is happening in such early stages of the evolution of planetary systems”. In fact, for the new measurements of the planetary masses, it was necessary to separate the signals generated by these planets from the signal generated by the star's activity, which is almost ten times larger. At this point, the specialisation of STELLA (STELLar Activity) comes into play. “With its large wavelength coverage from ultraviolet to infrared radiation at a high spectral resolution, STELLA can track the magnetic activity of a star,” adds Professor Klaus Strassmeier, director of the research branch Cosmic Magnetic Fields at AIP and PI for STELLA.

The study shows that the masses and radii of the planets V1298 Tau b and c are surprisingly similar to those of the giant planets of the Solar System or in other old extrasolar systems. These measurements, which are the first to be obtained of such young giant planets, allow scientists to test current ideas about the formation of planetary systems. “For many years, theoretical models have indicated that giant planets begin their evolution as bodies with a larger size, and that they later contract over hundreds of million or even billions of years,” explains Dr Víctor J. Sánchez Béjar, researcher at the IAC and co-author of the work. “We now know that they can actually reach a size similar to that of the planets in the solar system in a very short time,” he notes.

The study of young systems gives researchers clues about what happened during the infancy of our solar system. “We still do not know if V1298 Tau and its planets are a normal case and whether their evolution is similar to that of most planets or if we are facing an exceptional case; if this were the normal scenario, it would mean that the evolution of planets like Jupiter and Saturn could have been very different from what we think,” comments Dr Nicolas Lodieu, a researcher at the IAC, former PhD student at AIP and also a co-author of the work. The results of this work thus help to build a more solid idea of the early evolution of planetary systems like ours.

To achieve the measurement of these masses, the study has required a significant observational effort and the collaboration of multiple observatories and institutions from different countries. It was necessary to combine radial velocity measurements from various instruments such as the high-resolution HARPS-N ultrastable spectrograph at the Roque de los Muchachos Observatory's (ORM) Telescopio Nazionale Galileo (TNG); the CARMENES high resolution spectrograph at the Calar Alto observatory; the HERMES spectrograph on the Mercator telescope, also at the ORM; and the SES spectrograph at AIP’s STELLA telescopes at the Teide Observatory. Observations taken from the Las Cumbres Observatory have been used to continuously monitor the variations of the star's activity.





Further information:

Original publication

Rapid contraction of giant planets orbiting the 20 million-years old star V1298 Tau


https://www.nature.com/articles/s41550-021-01533-7

IAC press release

https://www.iac.es/en/outreach/news/study-reveals-giant-planets-could-reach-maturity-much-earlier-previously-thought

More about STELLA

https://www.aip.de/en/stella/



Contacts:

Prof. Dr. Klaus Strassmeier
Science contact
Phone: +49 331 7499 295

kstrassmeier@aip.de

Saturday, October 16, 2021

Hubble Finds Evidence of Persistent Water Vapour Atmosphere on Europa

Hubble's View of Jupiter and Europa in August 2020 
 
Artist’s Impression of Jupiter and Europa 
 
Artist’s Impression of Jupiter and Europa 
 
Artist’s Impression of a Water Atmosphere on Europa 
 
Galileo Spacecraft’s Image of Europa




Videos

Space Sparks Episode 7
Space Sparks Episode 7



Observations by the NASA/ESA Hubble Space Telescope recently revealed water vapour in the atmosphere of Ganymede, one of Jupiter’s moons. A new analysis of archival images and spectra has now revealed that water vapour is also present in the atmosphere of Jupiter’s icy moon Europa. The analysis found that a water vapour atmosphere is present only on one hemisphere of the moon. This result advances our understanding of the atmospheric structure of icy moons, and helps lay the groundwork for upcoming science missions which will explore Jupiter’s icy moons.

Europa — one of Jupiter’s 79 moons — is both the sixth closest moon to Jupiter and the sixth largest moon in the Solar System. It is an icy orb larger than the dwarf planet Pluto with a smooth, icy surface scarred by cracks and fissures. The surface of the moon is a bleak environment with an average temperature of −170 °C and only a tenuous atmosphere. However, astronomers suspect that Europa harbours a vast ocean underneath its icy surface, which some scientists speculate could host extraterrestrial life [1]. Now, for the first time, an astronomer has discovered evidence for persistent water vapour in the atmosphere of Europa.

Using a technique that recently resulted in the discovery of water vapour in the atmosphere of Jupiter’s moon Ganymede, an astronomer has found evidence of water in Europa’s trailing hemisphere — the portion of the moon that is always opposite to its direction of motion [2]. The asymmetric distribution of water vapour was predicted by previous studies based on computer simulations, but had not previously been detected observationally.

“The observation of water vapour on Ganymede and on the trailing side of Europa advances our understanding of the atmospheres of icy moons,” commented Lorenz Roth of the KTH Royal Institute of Technology in Stockholm, Sweden, the author of this study. “The detection of a stable H2O abundance on Europa is surprising because the surface temperatures are so low.”

To make this discovery, Roth delved into archival Hubble datasets, selecting ultraviolet observations of Europa from 1999, 2012, 2014 and 2015 while the moon was at various orbital positions. These observations were all taken with one of Hubble’s most versatile instruments — the Space Telescope Imaging Spectrograph (STIS). These ultraviolet STIS observations allowed Roth to determine the abundance of oxygen — one of the constituents of water — in Europa’s atmosphere, and by interpreting the strength of emission at different wavelengths he was able to infer the presence of water vapour. 

Previous observations of water vapour on Europa have been associated with transient plumes erupting through the ice, analogous to geysers here on Earth but more than 100 kilometres high. The phenomena seen in these plume studies were apparently transient inhomogeneities or blobs in the atmosphere. The new results, however, show similar amounts of water vapour to be present spread over a larger area in observations spanning from 1999 to 2015. This suggests the long-term presence of a water vapour atmosphere on Europa’s trailing hemisphere. Despite the presence of water vapour on Europa’s trailing hemisphere there is no indication of H2O on the leading hemisphere of Europa.

Space scientists working to understand these icy moons will soon be able to benefit from a close-up view. ESA’s  JUpiter ICy moons Explorer (JUICE) mission is being prepared for a tour of Ganymede, Callisto and Europa, Jupiter’s three largest icy moons. JUICE is the first large-class mission in ESA's Cosmic Vision 2015–2025 programme and is expected to launch in 2022 and arrive at Jupiter in 2031. The probe will carry an advanced suite of instruments — the most powerful remote sensing payload ever flown to the outer Solar System — and will spend at least three years making detailed observations of the Jovian system. Europa will also be visited by a NASA mission, Europa Clipper, which will perform a series of flybys of the moon and investigate its habitability, as well as selecting a landing site for a future mission.

“This result lays the groundwork for future science based on upcoming missions to the Jovian moons,” concluded Roth. “The more we can understand about these icy moons before spacecraft like JUICE and Europa Clipper arrive, the better use we can make of our limited observing time within the Jovian system.”

This discovery and the insights from upcoming missions such as JUICE will improve our understanding of potentially habitable environments in the Solar System. Understanding the formation and evolution of Jupiter and its moons also helps astronomers gain insights into Jupiter-like exoplanets around other stars. Combined with observations from space telescopes such as the upcoming NASA/ESA/CSA James Webb Space Telescope, this could help astronomers determine if life could emerge in Jupiter-like exoplanetary systems elsewhere in the universe.



Notes

[1] Liquid water is a crucial ingredient in the complex chemistry that underpins all known forms of life. Europa’s subsurface ocean is warmed not by sunlight, but rather by the subtle flexing of the moon caused by Jupiter’s immense gravitational field. The presence of liquid water and a source of energy make Europa one of the most likely locations in the Solar System for potential habitability.

[2] Europa is tidally locked, which means that it takes the same amount of time to revolve on its own axis as it does to orbit Jupiter. This means that the same hemisphere of Europa always faces Jupiter, and that the same hemisphere of the moon is always facing away from the direction that Europa is travelling along its orbit. Earth’s Moon is also tidally locked, which is why we always see the same face of the Moon in the night sky.




More Information

The Hubble Space Telescope is a project of international cooperation between ESA and NASA.

The astronomer who carried out this study was Lorenz Roth of the Royal Institute of Technology, Space and Plasma Physics, Sweden.

These results have been published in the journal Geophysical Research Letters.

Image credit: NASA, ESA, A. Simon (Goddard Space Flight Center), and M. H. Wong (University of California, Berkeley) and the OPAL team.



Links

Lorenz Roth
KTH Royal Institute of Technology
Stockholm, Sweden
Email:
lorenzr@kth.se

Bethany Downer
ESA/Hubble Chief Science Communications Officer
Email:
Bethany.Downer@esahubble.org

Source: ESA/Hubble/News


Wednesday, July 28, 2021

Hubble Finds First Evidence of Water Vapour at Jupiter’s Moon Ganymede

Hubble’s View of Ganymede in 1996
 
Hubble’s Ultraviolet Observations of Ganymede in 1998
 
Artist’s Impression of Ganymede
 
Artist’s Impression of Ganymede
 
Artist’s Impression of a Sublimated Water Atmosphere on Ganymede
 
NASA’s Juno Spacecraft Observation of Ganymede in June 2021



Videos

Space Sparks Episode 4
Space Sparks Episode 4 
 
Artist’s Impression of Ganymede
Artist’s Impression of Ganymede


Astronomers have used archival datasets from the NASA/ESA Hubble Space Telescope to reveal the first evidence for water vapour in the atmosphere of Jupiter’s moon Ganymede, the result of the thermal escape of water vapour from the moon’s icy surface.

Jupiter’s moon Ganymede is the largest moon — and the ninth-largest object — in the Solar System. It may hold more water than all of Earth's oceans, but temperatures there are so cold that water on the surface freezes and the ocean lies roughly 160 kilometres below the crust. Nevertheless, where there is water there could be life as we know it. Identifying liquid water on other worlds is crucial in the search for habitable planets beyond Earth. And now, for the first time, evidence has been found for a sublimated water atmosphere on the icy moon Ganymede.

In 1998,  Hubble’s Space Telescope Imaging Spectrograph (STIS) took the first ultraviolet (UV) pictures of Ganymede, which revealed a particular pattern in the observed emissions from the moon’s atmosphere. The moon displays auroral bands that are somewhat similar to the auroral ovals observed on Earth and other planets with magnetic fields. These images were therefore illustrative evidence that Ganymede has a permanent magnetic field. The similarities between the two ultraviolet observations were explained by the presence of molecular oxygen, O2. The differences were explained at the time by the presence of atomic oxygen, O, which produces a signal that affects one UV colour more than the other. 

As part of a large observing programme to support NASA’s Juno mission in 2018, Lorenz Roth, of the KTH Royal Institute of Technology in Stockholm, Sweden, led a team that set out to capture UV spectra of Ganymede with Hubble’s Cosmic Origins Spectrograph (COS) instrument to measure the amount of atomic oxygen. They carried out a  combined analysis of new spectra taken in 2018 with the COS and archival images from the STIS instrument from 1998 and 2010. To their surprise, and in contrast to the original interpretations of the data from 1998, they discovered there was hardly any atomic oxygen in Ganymede's atmosphere. This means there must be another explanation for the apparent differences between the UV aurora images.

The explanation was then uncovered by Roth and his team in the relative distribution of the aurorae in the two images. Ganymede's surface temperature varies strongly throughout the day, and around noon near the equator it may become sufficiently warm that the icy surface releases some small amounts of water molecules. In fact, the perceived differences between the UV images are directly correlated with where water would be expected in the moon’s atmosphere. 

“Initially only the O2 had been observed,” explained Roth. “This is produced when charged particles erode the ice surface. The water vapour that we have now measured originates from ice sublimation caused by the thermal escape of H2O vapour from warm icy regions.”

This finding adds anticipation to ESA’s upcoming JUpiter ICy moons Explorer (JUICE) mission — the first large-class mission in ESA's Cosmic Vision 2015–2025 programme. Planned for launch in 2022 and arrival at Jupiter in 2029, it will spend at least three years making detailed observations of Jupiter and three of its largest moons, with particular emphasis on Ganymede as a planetary body and potential habitable world. Ganymede was identified for detailed investigation because it provides a natural laboratory for the analysis of the nature, evolution and potential habitability of icy worlds in general and the role it plays within the system of Galilean satellites, and its unique magnetic and plasma interactions with Jupiter and its environment (known as the Jovian system).

“Our results can provide the JUICE instrument teams with valuable information that may be used to refine their observation plans to optimise the use of the spacecraft,” added Roth. 

Understanding the Jovian system and unravelling its history, from its origin to the possible emergence of habitable environments, will provide us with a better understanding of how gas giant planets and their satellites form and evolve. In addition, new insights will hopefully be found into the potential for the emergence of life in Jupiter-like exoplanetary systems.




More Information

The Hubble Space Telescope is a project of international cooperation between ESA and NASA.

This image was taken as part of the HST observation programs GO-7939 (PI: H. Moos), GO-12244 (PI: J. Saur), and GO-14634 (PI: D. Grodent).

The results have been published in Nature Astronomy. The international team behind this paper consists of L. Roth (KTH Royal Institute of Technology, Sweden), N. Ivchenko (KTH Royal Institute of Technology, Sweden), G. R. Gladstone (Southwest Research Institute, Texas, USA), J. Saur (Institut für Geophysik und Meteorologie, Germany), D. Grodent (Laboratoire de Physique Atmosphérique et Planétaire, Belgium), B. Bonfond (Laboratoire de Physique Atmosphérique et Planétaire, Belgium), P. M. Molyneux (Southwest Research Institute, Texas, USA), and K. D. Retherford (Southwest Research Institute, Texas, USA).



Links

Lorenz Roth
KTH Royal Institute of Technology
Stockholm, Sweden
Email:
lorenzr@kth.se

Bethany Downer
ESA/Hubble Chief Communications Officer
Email:
Bethany.Downer@esahubble.org

Source:ESA/News


Wednesday, March 24, 2021

Pandora Mission Would Expand NASA’s Capabilities in Probing Alien Worlds

This illustration captures an exoplanet as it is about to cross in front of – or transit – its start
Credit: NASA's Goddard Space Flight Center.
Hi-res image

This illustration (not to scale) depicts Pandora’s orbital pattern in Sun-synchronous low-Earth orbit, located approximately 435 to 497 miles (700 to 800 kilometers) above Earth’s surface, as it observes its targeted exoplanets and stars. This orbit enables Pandora to obtain multiple observations of exoplanets over long periods and the Earthshine exclusion zone helps avoid reflected light from Earth. Credits: Lawrence Livermore National Laboratory and NASA’s Goddard Space Flight Center.
Hi-res image

This illustration depicts Pandora’s use of transit spectroscopy to reliably identify an exoplanet’s atmospheric composition as it passes in front of its host star. Credits: Lawrence Livermore National Laboratory and NASA’s Goddard Space Flight Center.
Hi-res image

In the quest for habitable planets beyond our own, NASA is studying a mission concept called Pandora, which could eventually help decode the atmospheric mysteries of distant worlds in our galaxy. One of four low-cost astrophysics missions selected for further concept development under NASA’s new Pioneers program, Pandora would study approximately 20 stars and exoplanets – planets outside of our solar system – to provide precise measurements of exoplanetary atmospheres.

This mission would seek to determine atmospheric compositions by observing planets and their host stars simultaneously in visible and infrared light over long periods. Most notably, Pandora would examine how variations in a host star’s light impacts exoplanet measurements. This remains a substantial problem in identifying the atmospheric makeup of planets orbiting stars covered in starspots, which can cause brightness variations as a star rotates.

Pandora is a small satellite mission known as a SmallSat, one of three such orbital missions receiving the green light from NASA to move into the next phase of development in the Pioneers program. SmallSats are low-cost spaceflight missions that enable the agency to advance scientific exploration and increase access to space. Pandora would operate in Sun-synchronous low-Earth orbit, which always keeps the Sun directly behind the satellite. This orbit minimizes light changes on the satellite and allows Pandora to obtain data over extended periods. Of the SmallSat concepts selected for further study, Pandora is the only one focused on exoplanets.

“Exoplanetary science is moving from an era of planet discovery to an era of atmospheric characterization,” said Elisa Quintana, an astrophysicist at NASA’s Goddard Space Flight Center in Greenbelt, Maryland, and the principal investigator for Pandora. “Pandora is focused on trying to understand how stellar activity affects our measurements of exoplanet atmospheres, which will lay the groundwork for future exoplanet missions aiming to find planets with Earth-like atmospheres.”

Maximizing the scientific potential

Pandora concentrates on studying exoplanetary and stellar atmospheres by surveying planets as they cross in front of – or transit – their host stars. To accomplish this, Pandora would take advantage of a proven technique called transit spectroscopy, which involves measuring the amount of starlight filtering through a planet’s atmosphere, and splitting it into bands of color known as a spectrum. These colors encode information that helps scientists identify gases present in the planet’s atmosphere, and can help determine if a planet is rocky with a thin atmosphere like Earth or if it has a thick gas envelope like Neptune.

This mission, however, would take transit spectroscopy a step further. Pandora is designed to mitigate one of the technique’s most crucial setbacks: stellar contamination. “Stars have atmospheres and changing surface features like spots that affect our measurements,” said Jessie Christiansen, the deputy science lead at the NASA Exoplanet Archive at Caltech in Pasadena, California, and a co-investigator for Pandora. “To be sure we’re really observing an exoplanet’s atmosphere, we need to untangle the planet’s variations from those of the star.”

Pandora would separate stellar and exoplanetary signals by observing them simultaneously in infrared and visible light. Stellar contamination is easier to detect at the shorter wavelengths of visible light, and so obtaining atmospheric data through both infrared and visible light would allow scientists to better differentiate observations coming from exoplanet atmospheres and stars.

“Stellar contamination is a sticking point that complicates precise observations of exoplanets,” said Benjamin Rackham, a 51 Pegasi b Postdoctoral Fellow at the Massachusetts Institute of Technology in Cambridge and a co-investigator for Pandora. “Pandora would help build the necessary tools for disentangling stellar and planetary signals, allowing us to better study the properties of both starspots and exoplanetary atmospheres.”

Sinergy in space

Joining forces with NASA’s larger missions, Pandora would operate concurrently with the James Webb Space Telescope, slated for launch later this year. Webb will provide the ability to study the atmospheres of exoplanets as small as Earth with unprecedented precision, and Pandora would seek to expand the telescope’s research and findings by observing the host stars of previously identified planets over longer periods.

Missions such as NASA’s Transiting Exoplanet Survey Satellite (TESS), Hubble Space Telescope, and the retired Kepler and Spitzer spacecraft have given scientists astonishing glimpses at these distant worlds, and laid a strong foundation in exoplanetary knowledge. These missions, however, have yet to fully address the stellar contamination problem, the magnitude of which is uncertain in previous studies of exoplanetary atmospheres. Pandora seeks to fill these critical gaps in NASA’s understanding of planetary atmospheres and increase the capabilities in exoplanet research. 

“Pandora is the right mission at the right time because thousands of exoplanets have already been discovered, and we are aware of many that are amenable to atmospheric characterization that orbit small active stars,” said Jessie Dotson, an astrophysicist at NASA’s Ames Research Center in California’s Silicon Valley and the deputy principal investigator for Pandora. “The next frontier is to understand the atmospheres of these planets, and Pandora would play a key role in uncovering how stellar activity impacts our ability to characterize atmospheres. It would be a great complement to Webb’s mission.”

A launch pad for exploration

Lawrence Livermore National Laboratory (LLNL), in Livermore, California, is co-leading the Pandora mission with NASA’s Goddard Space Flight Center. LLNL will manage the mission and leverage capabilities developed for other government agencies, including a low-cost approach to the telescope design and fabrication that enables this groundbreaking exoplanet science from a SmallSat platform.

NASA’s Pioneers program, which consists of SmallSats, payloads attached to the International Space Station, and scientific balloon experiments, fosters innovative space and suborbital experiments for early-to-mid-career researchers through low-cost, small hardware missions. Under this new program, Pandora would operate on a five-year timeline with a budget cap of $20 million.

Despite tight constraints, the Pioneers program enables Pandora to concentrate on a focused research question while engaging a diverse team of students and early career scientists from more than a dozen of universities and research institutes. This SmallSat platform creates an excellent blueprint for small-scale missions to make an impact in the astrophysics community.

“Pandora’s long-duration observations in visible and infrared light are unique and well-suited for SmallSats,” said Quintana. “We are excited that Pandora will play a crucial role in NASA’s quest for finding other worlds that could potentially be habitable.”

For more information about the Pioneers program, visit:  https://science.nasa.gov/astrophysics/programs/astrophysics-pioneers

By Anisha Engineer
NASA’s Goddard Space Flight Center, Greenbelt, Md.

Media Contact:

Claire Andreoli
NASA’s Goddard Space Flight Center, Greenbelt, Md.

Editor: Rob Garner



Wednesday, February 17, 2021

Flipped-Over Exoplanets Prove New Disk-Tilt Mechanism

Figure 1: Conceptual illustration of the exoplanetary system K2-290. The central star (center) has two planets and a companion star (upper right). The two planets orbit around the central star in nearly the opposite direction to the star's spin. The innermost planet, about 75% the size of Neptune, orbits the star every nine days. The larger, Jupiter sized planet, requires more than 48 days for a round trip, still faster than Mercury in our own system with its 88 day orbit. (Credit: Christoffer Grønne/Aarhus University). Hi-res image

An international team including astronomers from Tokyo Institute of Technology and Aarhus University discovered evidence that in some cases protoplanetary disks, gas and dust disks surrounding young stars in which planets form, may have been flipped over, resulting in backwards or retrograde orbits of the planets. This finding is an important step in understanding planet formation and orbital evolution.

In the Solar System, the eight planets orbit in the same direction, this is also the same direction that the Sun rotates. Over the last decade researchers discovered that this is not always the case with exoplanets, planets which orbit around stars other than the Sun. Some exoplanets have orbits tilted wildly away from the rotation of the star. Some even have orbits tipped over backwards with respect to the central star. The mechanisms by which this wide diversity of orbits come to be is an important question in modern astronomy.

In one possible mechanism, while the planets are still forming in a protoplanetary disk of gas and dust around a young star, the gravity of a nearby companion star can tilt the disk so that the planets form on misaligned orbits from the beginning. Here, ‘nearby’ means within about a light-year. This disk-tilt mechanism was first proposed in 2012, but no confirmed examples had been observed until now.

The exoplanetary system, K2-290, is an ideal laboratory to test this disk-tilt mechanism. It has a nearby companion star identified by the Subaru Telescope (Note 1). It also has two planets with coplanar orbits, orbits that are aligned with each other. The presence of two planets with similar orbits is important because it rules out scenarios where interactions between the planets cause the orbits to tilt.

The team including Dr. Teruyuki Hirano (Tokyo Institute of Technology/National Institutes of Natural Sciences) and Dr. Maria Hjorth (Aarhus University/Tokyo Institute of Technology) used the Subaru Telescope and other telescopes (Note 2) to measure the misalignment between the orbits of the planets and the central star. They found that the planet’s orbits have flipped over nearly backwards. Numerical simulations by the team showed that the companion would have been able to flip over the protoplanetary disk, imparting retrograde orbits on the resulting planets. This provides strong evidence that the disk-tilt mechanism could be responsible for misaligned orbits, not just in this case, but in other exoplanet systems as well. It is no longer safe to assume that planetary orbits are initially aligned with the rotation of the star just after the formation of the planets in their disk. While other theories to explain spin-orbit misalignments in exoplanet systems tend to work best on large, Jupiter-like planets in short period orbits, the disk-tilt mechanism applies to planets of any size; even potentially habitable Earth-sized planets.


These results appeared as Hjorth et. al. "A backward-spinning star with two coplanar planets" in the Proceedings of the National Academy of Sciences of the United States of America on February 15, 2021.

References:

Note 1: The companion star was discovered in 2018 using IRCS on the Subaru Telescope. The result appeared as Hjorth et al. "K2-290: a warm Jupiter and a mini-Neptune in a triple-star system" in Monthly Notices of the Royal Astronomical Society on January 15, 2019.

Note 2: The observations were made in 2019 using three high-dispersion spectrographs: HDS on the Subaru Telescope, HARPS-N on the Telescopio Nazionale Galileo, and ESPRESSO on the VLT. The alignments between the two planets' orbits and the star's rotation were measured using the Rossiter-McLaughlin (RM) effect. See "
Inclined Orbits Prevail in Exoplanetary Systems" (press release on January 12, 2011) for other examples of misaligned exoplanet systems measured with the RM effect.

 

 Source: Subaru Telescope



Tuesday, January 26, 2021

Puzzling six-exoplanet system with rhythmic movement challenges theories of how planets form

An artist’s view of the TOI-178 planetary system 
 
Location of the TOI-178 planetary system in the constellation of Sculptor



Videos

ESOcast 233 Light: Six-Exoplanet System with Rhythmic Movement Challenges Theories of How Planets Form
ESOcast 233 Light: Six-Exoplanet System with Rhythmic Movement Challenges Theories of How Planets Form 
 
Artist’s animation of the TOI-178 orbits and resonances (sound on!)
Artist’s animation of the TOI-178 orbits and resonances (sound on!) 
 
Animated artist’s impression of the six-exoplanet system
Animated artist’s impression of the six-exoplanet system 
 
ESOcast 233 Light: Six-Exoplanet System with Rhythmic Movement Challenges Theories of How Planets Form
ESOcast 233 Light: Six-Exoplanet System with Rhythmic Movement Challenges Theories of How Planets Form 
 
Artist’s animation of the TOI-178 orbits and resonances (sound on!)
Artist’s animation of the TOI-178 orbits and resonances (sound on!) 
 
Animated artist’s impression of the six-exoplanet system
Animated artist’s impression of the six-exoplanet system


 

Using a combination of telescopes, including the Very Large Telescope of the European Southern Observatory (ESO’s VLT), astronomers have revealed a system consisting of six exoplanets, five of which are locked in a rare rhythm around their central star. The researchers believe the system could provide important clues about how planets, including those in the Solar System, form and evolve.

The first time the team observed TOI-178, a star some 200 light-years away in the constellation of Sculptor, they thought they had spotted two planets going around it in the same orbit. However, a closer look revealed something entirely different. “Through further observations we realised that there were not two planets orbiting the star at roughly the same distance from it, but rather multiple planets in a very special configuration,” says Adrien Leleu from the Université de Genève and the University of Bern, Switzerland, who led a new study of the system published today in Astronomy & Astrophysics.

The new research has revealed that the system boasts six exoplanets and that all but the one closest to the star are locked in a rhythmic dance as they move in their orbits. In other words, they are in resonance. This means that there are patterns that repeat themselves as the planets go around the star, with some planets aligning every few orbits. A similar resonance is observed in the orbits of three of Jupiter’s moons: Io, Europa and Ganymede. Io, the closest of the three to Jupiter, completes four full orbits around Jupiter for every orbit that Ganymede, the furthest away, makes, and two full orbits for every orbit Europa makes.

The five outer exoplanets of the TOI-178 system follow a much more complex chain of resonance, one of the longest yet discovered in a system of planets. While the three Jupiter moons are in a 4:2:1 resonance, the five outer planets in the TOI-178 system follow a 18:9:6:4:3 chain: while the second planet from the star (the first in the resonance chain) completes 18 orbits, the third planet from the star (second in the chain) completes 9 orbits, and so on. In fact, the scientists initially only found five planets in the system, but by following this resonant rhythm they calculated where in its orbit an additional planet would be when they next had a window to observe the system.

More than just an orbital curiosity, this dance of resonant planets provides clues about the system’s past. “The orbits in this system are very well ordered, which tells us that this system has evolved quite gently since its birth,” explains co-author Yann Alibert from the University of Bern. If the system had been significantly disturbed earlier in its life, for example by a giant impact, this fragile configuration of orbits would not have survived.

Disorder in the rhythmic system

But even if the arrangement of the orbits is neat and well-ordered, the densities of the planets “are much more disorderly,” says Nathan Hara from the Université de Genève, Switzerland, who was also involved in the study. “It appears there is a planet as dense as the Earth right next to a very fluffy planet with half the density of Neptune, followed by a planet with the density of Neptune. It is not what we are used to.” In our Solar System, for example, the planets are neatly arranged, with the rocky, denser planets closer to the central star and the fluffy, low-density gas planets farther out.

“This contrast between the rhythmic harmony of the orbital motion and the disorderly densities certainly challenges our understanding of the formation and evolution of planetary systems,” says Leleu.

Combining techniques

To investigate the system’s unusual architecture, the team used data from the European Space Agency’s CHEOPS satellite, alongside the ground-based ESPRESSO instrument on ESO’s VLT and the NGTS and SPECULOOS, both sited at ESO’s Paranal Observatory in Chile. Since exoplanets are extremely tricky to spot directly with telescopes, astronomers must instead rely on other techniques to detect them. The main methods used are imaging transits — observing the light emitted by the central star, which dims as an exoplanet passes in front of it when observed from the Earth — and radial velocities — observing the star’s light spectrum for small signs of wobbles which happen as the exoplanets move in their orbits. The team used both methods to observe the system: CHEOPS, NGTS and SPECULOOS for transits and ESPRESSO for radial velocities. 

By combining the two techniques, astronomers were able to gather key information about the system and its planets, which orbit their central star much closer and much faster than the Earth orbits the Sun. The fastest (the innermost planet) completes an orbit in just a couple of days, while the slowest takes about ten times longer. The six planets have sizes ranging from about one to about three times the size of Earth, while their masses are 1.5 to 30 times the mass of Earth. Some of the planets are rocky, but larger than Earth — these planets are known as Super-Earths. Others are gas planets, like the outer planets in our Solar System, but they are much smaller — these are nicknamed Mini-Neptunes.

Although none of the six exoplanets found lies in the star's habitable zone, the researchers suggest that, by continuing the resonance chain, they might find additional planets that could exist in or very close to this zone. ESO’s Extremely Large Telescope (ELT), which is set to begin operating this decade, will be able to directly image rocky exoplanets in a star’s habitable zone and even characterise their atmospheres, presenting an opportunity to get to know systems like TOI-178 in even greater detail.




More Information

This research was presented in the paper “Six transiting planets and a chain of Laplace resonances in TOI-178” to appear in Astronomy & Astrophysics (doi: 10.1051/0004-6361/202039767).

The team is composed of A. Leleu (Observatoire Astronomique de l’Université de Genève, Switzerland [UNIGE], University of Bern, Switzerland [Bern]), Y. Alibert (Bern), N. C. Hara (UNIGE), M. J. Hooton (Bern), T. G. Wilson (Centre for Exoplanet Science, SUPA School of Physics and Astronomy, University of St Andrews, UK [St Andrews]), P. Robutel (IMCCE, UMR8028 CNRS, Observatoire de Paris, France [IMCCE]), J.-B Delisle (UNIGE), J. Laskar (IMCCE), S. Hoyer (Aix Marseille Univ, CNRS, CNES, LAM, France [AMU]), C. Lovis (UNIGE), E. M. Bryant (Department of Physics, University of Warwick, UK [Warwick], Centre for Exoplanets and Habitability, University of Warwick [CEH]), E. Ducrot (Astrobiology Research Unit, Université de Liège, Belgium [Liège]), J. Cabrera (Institute of Planetary Research, German Aerospace Center (DLR), Berlin, Germany [Institute of Planetary Research, DLR]), J. Acton (School of Physics and Astronomy, University of Leicester, UK [Leicester]), V. Adibekyan (Instituto de Astrofísica e Ciências do Espaço, Universidade do Porto, Portugal [IA], Centro de Astrofísica da Universidade do Porto, Departamento de Física e Astronomia, Universidade do Porto [CAUP]), R. Allart (UNIGE), C, Allende Prieto (Instituto de Astrofísica de Canarias, Tenerife [IAC], Departamento de Astrofísica, Universidad de La Laguna, Tenerife [ULL]), R. Alonso (IAC, ULL), D. Alves (Camino El Observatorio 1515, Las Condes, Santiago, Chile), D. R Anderson (Warwick, CEH), D. Angerhausen (ETH Zürich, Institute for Particle Physics and Astrophysics), G. Anglada Escudé (Institut de Ciències de l’Espai [ICE, CSIC], Bellaterra, Spain, Institut d’Estudis Espacials de Catalunya [IEEC], Barcelona, Spain), J. Asquier (ESTEC, ESA, Noordwijk, the Netherlands [ESTEC]), D. Barrado (Depto. de Astrofísica, Centro de Astrobiologia [CSIC-INTA], Madrid, Spain), S.C.C Barros (IA, Departamento de Física e Astronomia, Universidade do Porto), W. Baumjohann (Space Research Institute, Austrian Academy of Sciences, Austria), D. Bayliss (Warwick, CEH), M. Beck (UNIGE), T. Beck (Bern) A. Bekkelien (UNIGE), W. Benz (Bern, Center for Space and Habitability, Bern, Switzerland [CSH]), N. Billot (UNIGE), A. Bonfanti (IWF), X. Bonfils (Université Grenoble Alpes, CNRS, IPAG, Grenoble, France), F. Bouchy (UNIGE), V. Bourrier (UNIGE), G. Boué (IMCCE), A. Brandeker (Department of Astronomy, Stockholm University, Sweden), C. Broeg (Bern), M. Buder (Institute of Optical Sensor Systems, German Aerospace Center (DLR) [Institute of Optical Sensor Systems, DLR]), A. Burdanov (Liège, Department of Earth, Atmospheric and Planetary Science, Massachusetts Institute of Technology, USA), M. R. Burleigh (Leicester), T. Bárczy (Admatis, Miskok, Hungary), A. C. Cameron (St Andrews), S. Chamberlain (Leicester), S. Charnoz (Université de Paris, Institut de physique du globe de Paris, CNRS, France), B. F. Cooke (Warwick, CEH), C. Corral Van Damme (ESTEC), A. C. M. Correia (CFisUC, Department of Physics, University of Coimbra, Portugal, IMCCE, UMR8028 CNRS, Observatoire de Paris, France), S. Cristiani (INAF - Osservatorio Astronomico di Trieste, Italy [INAF Trieste]), M. Damasso (INAF - Osservatorio Astrofisico di Torino, Italy [INAF Torino]), M. B. Davies (Lund Observatory, Dept. of Astronomy and Theoretical Physics, Lund University, Sweden), M. Deluil (AMU), L. Delrez (AMU, Space sciences, Technologies and Astrophysics Research [STAR] Institute, Université de Liège, Belgium, UNIGE), O. D. S. Demangeon (IA), B.-O. Demory (CSH), P. Di Marcantonio (INAF Trieste), G. Di. Persio (INAF, Istituto di Astrofisica e Planetologia Spaziali, Roma, Italy), X. Dumusque (UNIGE), D. Ehrenreich (UNIGE), A. Erikson (Institute of Planetary Research, DLR), P. Figueira (Instituto de Astrofísica e Ciências do Espaço, Universidade do Porto, ESO Vitacura), A. Fortier (Bern, CSH), L. Fossato (Space Research Institute, Austrian Academy of Sciences, Graz, Austria [IWF]), M. Fridlund (Leiden Observatory, University of Leiden, The Netherlands, Department of Space, Earth and Environment, Chalmers University of Technology, Onsala Space Observatory, Sweden [Chalmers]), D. Futyan (UNIGE), D. Gandolfi (Dipartimento di Fisica, Università degli Studi di Torino, Italy), A. García Muñoz (Center for Astronomy and Astrophysics, Technical University Berlin, Germany), L. Garcia (Liège), S. Gill (Warwick, CEH), E. Gillen (Astronomy Unit, Queen Mary University of London, UK, Cavendish Laboratory, Cambridge, UK [Cavendish Laboratory]), M. Gillon (Liège), M. R. Goad (Leicester), J. I. González Hernández (IAC, ULL), M. Guedel (University of Vienna, Department of Astrophysics, Austria), M. N. Günther (Department of Physics and Kavli Institute for Astrophysics and Space Research, Massachusetts Institute of Technology, USA), J. Haldemann (Bern), B. Henderson (Leicester), K. Heng (CSH), A. E. Hogan (Leicester), E. Jehin (STAR), J. S. Jenkins (Departamento de Astronomía, Universidad de Chile, Santiago, Chile, Centro de Astrofísica y Tecnologías Afines (CATA), Santiago, Chile), A. Jordán (Facultad de Ingeniería y Ciencias, Universidad Adolfo Ibáñez, Santiago, Chile, Millennium Institute for Astrophysics, Chile), L. Kiss (Konkoly Observatory, Research Centre for Astronomy and Earth Sciences, Budapest, Hungary), M. H. Kristiansen (Brorfelde Observatory, Observator Gyldenkernes, Denmark, DTU Space, National Space Institute, Technical University of Denmark, Denmark), K. Lam (Institute of Planetary Research, DLR), B. Lavie (UNIGE), A. Lecavelier des Etangs (Institut d’astrophysique de Paris, UMR7095 CNRS, Université Pierre & Marie Curie, Paris, France), M. Lendil (UNIGE), J. Lillo-Box (Depto. de Astrofísica, Centro de Astrobiologia (CSIC-INTA),ESAC campus, Madrid, Spain), G. Lo Curto (ESO Vitacura), D. Magrin (INAF, Osservatorio Astronomico di Padova, Italy [INAF Padova]), C. J. A. P. Martins (IA, CAUP), P. F. L. Maxted (Astrophysics Group, Keele University, UK), J. McCormac (Warwick), A. Mehner (ESO Vitacura), G. Micela (INAF - Osservatorio Astronomico di Palermo, Italy), P. Molaro (INAF Trieste, IFPU Trieste), M. Moyano (Instituto de Astronomía, Universidad Católica del Norte, Antofagasta, Chile), C. A. Murray (Cavendish Laboratory), V. Nascimbeni (INAF, Osservatorio Astronomico di Padova, Italy), N. J. Nunes (Instituto de Astrofísica e Ciências do Espaço, Faculdade de Ciências da Universidade de Lisboa, Portugal), G. Olofsson (Department of Astronomy, Stockholm University, Sweden), H. P. Osborn (CSH, Department of Physics and Kavli Institute for Astrophysics and Space Research, Massachusetts Institute of Technology, USA), M. Oshagh (IAC, ULL), R. Ottensamer (Department of Astrophysics, University of Vienna, Austria), I. Pagano (INAF, Osservatorio Astrofisico di Catania, Italy), E. Pallé (IAC, ULL), P. P. Pedersen  (Cavendish Laboratory), F. A. Pepe (UNIGE), C.M. Persson (Chalmers), G. Peter (Institute of Optical Sensor Systems, German Aerospace Center (DLR), Berlin, Germany), G. Piotto (INAF Padova, Dipartimento di Fisica e Astronomia "Galileo Galilei", Università degli Studi di Padova, Italy), G. Polenta (Space Science Data Center, Roma, Italy), D. Pollacco (Warwick), E. Poretti (Fundación G. Galilei – INAF (Telescopio Nazionale Galileo), La Palma, Spain, INAF - Osservatorio Astronomico di Brera, Merate, Italy), F. J. Pozuelos (Liège, STAR), F. Pozuelos (Liège, STAR), D. Queloz (UNIGE, Cavendish Laboratory), R. Ragazzoni (INAF Padova), N. Rando (ESTEC), F. Ratti (ESTEC), H. Rauer (Institute of Planetary Research, DLR), L. Raynard (Leicester), R. Rebolo (IAC, ULL), C. Reimers (Department of Astrophysics, University of Vienna, Austria), I. Ribas (Institut de Ciències de l’Espai (ICE, CSIC), Spain, Institut d’Estudis Espacials de Catalunya (IEEC), Barcelona, Spain), N. C. Santos (IA, Departamento de Física e Astronomia, Universidade do Porto), G. Scandariato (INAF, Osservatorio Astrofisico di Catania, Italy), J. Schneider (Paris Observatory, France), D. Sebastian (School of Physics Astronomy, University of Birmingham, UK [Birmingham]), M. Sestovic (CSH), A. E. Simon (Bern), A. M. S. Smith (Institute of Planetary Research, DLR), S. G. Sousa (IA), A. Sozzetti (INAF Torino), M. Steller (IWF), A. Suárez Mascareño (IAC, ULL), G. M. Szabó (ELTE Eötvös Loránd University, Gothard Astrophysical Observatory, Hungary, MTA-ELTE Exoplanet Research Group, Hungary), D Ségransan (UNIGE), N. Thomas (Bern), S. Thompson (Cavendish Laboratory), R. H. Tilbrook (Leicester), A. Triaud (Birmingham), S. Udry (UNIGE), V. Van Grootel (STAR), H. Venus (Institute of Optical Sensor Systems, DLR), F. Verrecchia (Space Science Data Center, ASI, Roma, Italy, INAF, Osservatorio Astronomico di Roma, Italy), J. I. Vines (Camino El Observatorio 1515, Santiago, Chile), N. A. Walton (Institute of Astronomy, University of Cambridge, UK), R. G. West (Warwick, CEH), P. K. Wheatley (Warwick, CEH), D. Wolter (Institute of Planetary Research, DLR), M. R. Zapatero Osorio (Centro de Astrobiología (CSIC-INTA), Madrid, Spain).

ESO is the foremost intergovernmental astronomy organisation in Europe and the world’s most productive ground-based astronomical observatory by far. It has 16 Member States: Austria, Belgium, the Czech Republic, Denmark, France, Finland, Germany, Ireland, Italy, the Netherlands, Poland, Portugal, Spain, Sweden, Switzerland and the United Kingdom, along with the host state of Chile and with Australia as a Strategic Partner. ESO carries out an ambitious programme focused on the design, construction and operation of powerful ground-based observing facilities enabling astronomers to make important scientific discoveries. ESO also plays a leading role in promoting and organising cooperation in astronomical research. ESO operates three unique world-class observing sites in Chile: La Silla, Paranal and Chajnantor. At Paranal, ESO operates the Very Large Telescope and its world-leading Very Large Telescope Interferometer as well as two survey telescopes, VISTA working in the infrared and the visible-light VLT Survey Telescope. Also at Paranal ESO will host and operate the Cherenkov Telescope Array South, the world’s largest and most sensitive gamma-ray observatory. ESO is also a major partner in two facilities on Chajnantor, APEX and ALMA, the largest astronomical project in existence. And on Cerro Armazones, close to Paranal, ESO is building the 39-metre Extremely Large Telescope, the ELT, which will become “the world’s biggest eye on the sky”.



Links

Adrien Leleu
Université de Genève
Geneva, Switzerland
Email:
Adrien.Leleu@unige.ch

Yann Alibert
University of Bern
Bern, Switzerland
Tel: +41 31 631 55 47
Email:
yann.alibert@space.unibe.ch

Nathan Hara
Université de Genève
Geneva, Switzerland
Tel: +41 22 379 24 14
Email:
nathan.hara@unige.ch

Bárbara Ferreira
ESO Public Information Officer
Garching bei München, Germany
Tel: +49 89 3200 6670
Cell: +49 151 241 664 00
Email:
press@eso.org

Source: ESO/News 


Thursday, November 05, 2020

Supersonic winds, rocky rains forecasted on lava planet News

Artist’s impression of the lava planet K2-141b. At the center of the large illuminated region there is an ocean of molten rock overlain by an atmosphere of rock vapour. Supersonic winds blow towards the frigid and airless nightside, condensing into rock rain and snow, which sluggishly flow back to the hottest region of the magma ocean.

“Rocky” weather could change the surface and atmosphere over time on exoplanet K2-141b

Among the most extreme planets discovered beyond the edges of our solar system are lava planets: fiery hot worlds that circle so close to their host star that some regions are likely oceans of molten lava. According to scientists from McGill University, York University, and the Indian Institute of Science Education, the atmosphere and weather cycle of at least one such exoplanet is even stranger, featuring the evaporation and precipitation of rocks, supersonic winds that rage over 5000 km/hr, and a magma ocean 100 km deep.

In a study published in Monthly Notices of the Royal Astronomical Society, the scientists use computer simulations to predict the conditions on K2-141b, an Earth-size exoplanet with a surface, ocean, and atmosphere all made up of the same ingredients: rocks. The extreme weather forecasted by their analysis could permanently change the surface and atmosphere of K2-141b over time.

“The study is the first to make predictions about weather conditions on K2-141b that can be detected from hundreds of light years away with next-generation telescopes such as the James Webb Space Telescope,” says lead author Giang Nguyen, a PhD student at York University who worked under the supervision of McGill University Professor Nicolas Cowan on the study.

Two-thirds of the exoplanet faces endless daylight

In analyzing the illumination pattern of the exoplanet, the team discovered that about two-thirds of K2-141b faces perpetual daylight – rather than the illuminated hemisphere we are used to on Earth. K2-141b belongs to a subset of rocky planets that orbit very close to their star. This proximity keeps the exoplanet gravitationally locked in place, meaning the same side always faces the star.

The night side experiences frigid temperatures of below -200 C. The day side of the exoplanet, at an estimated 3000 C, is hot enough to not only melt rocks but vaporize them as well, ultimately creating a thin atmosphere in some areas. “Our finding likely means that the atmosphere extends a little beyond the shore of the magma ocean, making it easier to spot with space telescopes,” says Nicolas Cowan, a professor in the Department of Earth & Planetary Sciences at McGill University.

Like Earth’s water cycle, only with rocks

Remarkably, the rock vapour atmosphere created by the extreme heat undergoes precipitation. Just like the water cycle on Earth, where water evaporates, rises into the atmosphere, condenses, and falls back as rain, so too does the sodium, silicon monoxide, and silicon dioxide on K2-141b. On Earth, rain flows back into the oceans, where it will once more evaporate and the water cycle is repeated. On K2-141b, the mineral vapour formed by evaporated rock is swept to the frigid night side by supersonic winds and rocks “rain” back down into a magma ocean. The resulting currents flow back to the hot day side of the exoplanet, where rock evaporates once more.

Still, the cycle on K2-141b is not as stable as the one on Earth, say the scientists. The return flow of the magma ocean to the day side is slow, and as a result they predict that the mineral composition will change over time – eventually changing the very surface and atmosphere of K2-141b.

“All rocky planets­, including Earth, started off as molten worlds but then rapidly cooled and solidified. Lava planets give us a rare glimpse at this stage of planetary evolution,” says Professor Cowan of the Department of Earth and Planetary Sciences.

The next step will be to test if these predictions are correct, say the scientists. The team now has data from the Spitzer Space Telescope that should give them a first glimpse at the day-side and night-side temperatures of the exoplanet. With the James Webb Space Telescope launching in 2021, they will also be able to verify whether the atmosphere behaves as predicted.

About the study

"Modelling the atmosphere of lava planet K2-141b: implications for low and high resolution spectroscopy" by T. Giang Nguyen, Nicolas Cowan, Agnibha Banerjee and John Moores is published in Monthly Notices of the Royal Astronomical Society.

DOI: http://dx.doi.org/10.1093/mnras/staa2487

About McGill University

Founded in Montreal, Quebec, in 1821, McGill University is Canada’s top ranked medical doctoral university. McGill is consistently ranked as one of the top universities, both nationally and internationally. It is a world-renowned institution of higher learning with research activities spanning two campuses, 11 faculties, 13 professional schools, 300 programs of study and over 40,000 students, including more than 10,200 graduate students. McGill attracts students from over 150 countries around the world, its 12,800 international students making up 31% of the student body. Over half of McGill students claim a first language other than English, including approximately 19% of our students who say French is their mother tongue.

http://www.mcgill.ca/newsroom/
http://twitter.com/McGillU

Contact Information:

Shirley Cardenas
Organization:
Media Relations Office, McGill University
Email: shirley.cardenas@mcgill.ca
Office Phone: (514) 398-6751
Mobile Phone: (514) 594-6877



Saturday, February 08, 2020

NASA's Webb Will Seek Atmospheres around Potentially Habitable Exoplanets

This artist’s concept portrays the seven rocky exoplanets within the Trappist-1 system, located 40 light-years from Earth. Astronomers will observe these worlds with Webb in an effort to detect the first atmosphere of an Earth-sized planet beyond our solar system. Credits: NASA and JPL/Caltec. Release Images

This month marks the third anniversary of the discovery of a remarkable system of seven planets known as TRAPPIST-1. These seven rocky, Earth-size worlds orbit an ultra-cool star 39 light-years from Earth. Three of those planets are in the habitable zone, meaning they are at the right orbital distance to be warm enough for liquid water to exist on their surfaces. After its 2021 launch, NASA’s James Webb Space Telescope will observe those worlds with the goal of making the first detailed near-infrared study of the atmosphere of a habitable-zone planet.

To find signs of an atmosphere, astronomers will use a technique called transmission spectroscopy. They observe the host star while the planet is crossing the face of the star, known as a transit. The light of the star filters through the planet’s atmosphere, which absorbs some of the starlight and leaves telltale fingerprints in the star’s spectrum.

Finding an atmosphere around a rocky exoplanet — the word scientists use for planets beyond our solar system — won’t be easy. Their atmospheres are more compact than those of gas giants, while their smaller size means they intercept less of the star’s light. TRAPPIST-1 is one of the best available targets for Webb since the star itself is also quite small, meaning the planets’ size relative to the star is larger.

“The atmospheres are harder to detect but the reward is higher. It would be very exciting to make the first detection of an atmosphere on an Earth-sized planet,” said David Lafrenière of the University of Montreal, principal investigator on one of the teams examining TRAPPIST-1.

Red dwarf stars like TRAPPIST-1 tend to have violent outbursts that could make the TRAPPIST-1 planets inhospitable. But determining whether they have atmospheres, and if so, what they're made of, is the next step to finding out whether life as we know it could survive on these distant worlds.

A coordinated effort

More than one team of astronomers will study the TRAPPIST-1 system with Webb. They plan to use a variety of instruments and observing modes to tease out as many details as they can for each planet in the system.

“It’s a coordinated effort because no one team could do everything we wanted to do with the TRAPPIST-1 system. The level of cooperation has been really spectacular,” explained Nikole Lewis of Cornell University, the principal investigator on one of the teams.

“With seven planets to choose from, we can each have a piece of the cake,” added Lafrenière.

Lafrenière’s program will target TRAPPIST-1d and -1f in an effort to not only detect an atmosphere but determine its basic composition. They expect to be able to distinguish between an atmosphere dominated by water vapor, or one composed mainly of nitrogen (like Earth) or carbon dioxide (like Mars and Venus).

Lewis’s program will observe TRAPPIST-1e with similar goals. TRAPPIST-1e is one of the planets beyond our solar system that has the most in common with Earth in terms of its density and the amount of radiation that it receives from its star. That makes it a great candidate for habitability — but scientists need to know more to find out.

A broad variety of planets

While the TRAPPIST-1 planets hold particular appeal from a standpoint of potential habitability, Lafrenière’s program will target a variety of planets — from rocky to mini-Neptunes to Jupiter-sized gas giants — at a variety of distances from their stars. The goal is to learn more about how, and where, these planets form.

In particular, astronomers continue to debate how gaseous planets can be found very close to their stars. Most believe that such a planet must have formed farther out in the protoplanetary disk — the disk around a star where planets are born — since more material is available far from the star, and then migrated inward. However, other scientists theorize that even large gas giants can form relatively close to their star.

“Also, maybe they formed farther out, but how much farther out?” asked Lewis.

To help inform the debate, astronomers will look at the ratio of carbon to oxygen in an assortment of exoplanets. This ratio can serve as a tracer of where a planet formed, because it varies with the distance from the star.

Weather maps

In addition to examining planets using transmission spectroscopy, the teams will also employ a technique known as a phase curve. This involves observing a planet over the course of an entire orbit, which is only practical for the hottest worlds with the shortest orbital periods.

A planet circling its star very close becomes tidally locked, meaning that it always shows the same face to the star, as the Moon does to Earth. As a result, distant observers watching the planet will see it go through various phases, since different sides of the planet are visible at different points in its orbit.

By measuring the planet at various times, astronomers can build up a map of the atmospheric temperature as a function of longitude. This technique was pioneered by NASA’s Spitzer Space Telescope, which made the first “weather map” of an exoplanet in 2007.

In addition, by observing the planet’s own heat emission, astronomers can model the atmosphere’s vertical structure.

“With a phase curve, we can build a complete 3D model of a planet’s atmosphere,” explained Lafrenière.

This work is being conducted as part of a Webb Guaranteed Time Observations (GTO) program. This program is designed to reward scientists who helped develop the key hardware and software components or technical and interdisciplinary knowledge for the observatory.

The James Webb Space Telescope will be the world’s premier space science observatory when it launches in 2021. Webb will solve mysteries in our solar system, look beyond to distant worlds around other stars, and probe the mysterious structures and origins of our universe and our place in it. Webb is an international program led by NASA with its partners, ESA (European Space Agency) and the Canadian Space Agency.