Showing posts with label hot super-earths. Show all posts
Showing posts with label hot super-earths. Show all posts

Saturday, May 11, 2024

NASA's Webb Hints at Possible Atmosphere Surrounding Rocky Exoplanet

Super-Earth Exoplanet 55 Cancri e (Artist’s Concept)
Credits: Illustration: NASA, ESA, CSA, Ralf Crawford (STScI)

Super-Earth Exoplanet 55 Cancri e (MIRI Secondary Eclipse Light Curve)
Credits: Illustration: NASA, ESA, CSA, Joseph Olmsted (STScI)
Science: Aaron Bello-Arufe (NASA-JPL)

Super-Earth Exoplanet 55 Cancri e (NIRCam + MIRI Emission Spectrum)
Credits: Illustration: NASA, ESA, CSA, Joseph Olmsted (STScI)
Science: Renyu Hu (NASA-JPL), Aaron Bello-Arufe (NASA-JPL), Michael Zhang (University of Chicago), Mantas Zilinskas (SRON)



Researchers using NASA’s James Webb Space Telescope may have detected atmospheric gases surrounding 55 Cancri e, a hot rocky exoplanet 41 light-years from Earth. This is the best evidence to date for the existence of any rocky planet atmosphere outside our solar system.

Renyu Hu from NASA’s Jet Propulsion Laboratory (JPL) in Pasadena, California, is lead author on a paper published today in Nature. “Webb is pushing the frontiers of exoplanet characterization to rocky planets,” Hu said. “It is truly enabling a new type of science.”

Super-Hot Super-Earth 55 Cancri e

55 Cancri e, also known as Janssen, is one of five known planets orbiting the Sun-like star 55 Cancri, in the constellation Cancer. With a diameter nearly twice that of Earth and density slightly greater, the planet is classified as a super-Earth: larger than Earth, smaller than Neptune, and likely similar in composition to the rocky planets in our solar system.

To describe 55 Cancri e as “rocky,” however, could leave the wrong impression. The planet orbits so close to its star (about 1.4 million miles, or one-twenty-fifth the distance between Mercury and the Sun) that its surface is likely to be molten – a bubbling ocean of magma. With such a tight orbit, the planet is also likely to be tidally locked, with a dayside that faces the star at all times and a nightside in perpetual darkness.

In spite of numerous observations since it was discovered to transit in 2011, the question of whether or not 55 Cancri e has an atmosphere – or even could have one given its high temperature and the continuous onslaught of stellar radiation and wind from its star – has gone unanswered.

“I’ve worked on this planet for more than a decade,” said Diana Dragomir, an exoplanet researcher at the University of New Mexico and co-author on the study. “It’s been really frustrating that none of the observations we’ve been getting have robustly solved these mysteries. I am thrilled that we're finally getting some answers!”

Unlike the atmospheres of gas giant planets, which are relatively easy to spot (the first was detected by NASA’s Hubble Space Telescope more than two decades ago), thinner and denser atmospheres surrounding rocky planets have remained elusive.

Previous studies of 55 Cancri e using data from NASA’s now-retired Spitzer Space Telescope suggested the presence of a substantial atmosphere rich in volatiles (molecules that occur in gas form on Earth) like oxygen, nitrogen, and carbon dioxide. But researchers could not rule out another possibility: that the planet is bare, save for a tenuous shroud of vaporized rock, rich in elements like silicon, iron, aluminum, and calcium. “The planet is so hot that some of the molten rock should evaporate,” explained Hu.

Measuring Subtle Variations in Infrared Colors

To distinguish between the two possibilities, the team used Webb’s NIRCam (Near-Infrared Camera) and MIRI (Mid-Infrared Instrument) to measure 4- to 12-micron infrared light coming from the planet.

Although Webb cannot capture a direct image of 55 Cancri e, it can measure subtle changes in light from the system as the planet orbits the star.

By subtracting the brightness during the secondary eclipse, when the planet is behind the star (starlight only), from the brightness when the planet is right beside the star (light from the star and planet combined), the team was able to calculate the amount of various wavelengths of infrared light coming from the dayside of the planet.

This method, known as secondary eclipse spectroscopy, is similar to that used by other research teams to search for atmospheres on other rocky exoplanets, like TRAPPIST-1 b.

Cooler than Expected

The first indication that 55 Cancri e could have a substantial atmosphere came from temperature measurements based on its thermal emission, or heat energy given off in the form of infrared light. If the planet is covered in dark molten rock with a thin veil of vaporized rock or no atmosphere at all, the dayside should be around 4,000 degrees Fahrenheit (~2,200 degrees Celsius).

“Instead, the MIRI data showed a relatively low temperature of about 2,800 degrees Fahrenheit [~1540 degrees Celsius],” said Hu. “This is a very strong indication that energy is being distributed from the dayside to the nightside, most likely by a volatile-rich atmosphere.” While currents of lava can carry some heat around to the nightside, they cannot move it efficiently enough to explain the cooling effect.

When the team looked at the NIRCam data, they saw patterns consistent with a volatile-rich atmosphere. “We see evidence of a dip in the spectrum between 4 and 5 microns — less of this light is reaching the telescope,” explained co-author Aaron Bello-Arufe, also from NASA JPL. “This suggests the presence of an atmosphere containing carbon monoxide or carbon dioxide, which absorb these wavelengths of light.” A planet with no atmosphere or an atmosphere consisting only of vaporized rock would not have this specific spectral feature.

“We’ve spent the last ten years modelling different scenarios, trying to imagine what this world might look like,” said co-author Yamila Miguel from the Leiden Observatory and the Netherlands Institute for Space Research (SRON). “Finally getting some confirmation of our work is priceless!”

Bubbling Magma Ocean

The team thinks that the gases blanketing 55 Cancri e would be bubbling out from the interior, rather than being present ever since the planet formed. “The primary atmosphere would be long gone because of the high temperature and intense radiation from the star,” said Bello-Arufe. “This would be a secondary atmosphere that is continuously replenished by the magma ocean. Magma is not just crystals and liquid rock; there’s a lot of dissolved gas in it, too.”

While 55 Cancri e is far too hot to be habitable, researchers think it could provide a unique window for studying interactions between atmospheres, surfaces, and interiors of rocky planets, and perhaps provide insights into the early conditions of Earth, Venus, and Mars, which are thought to have been covered in magma oceans far in the past. “Ultimately, we want to understand what conditions make it possible for a rocky planet to sustain a gas-rich atmosphere: a key ingredient for a habitable planet,” said Hu. This research was conducted as part of Webb’s General Observers (GO) Program 1952. Analysis of additional secondary eclipse observations of 55 Cancri e are currently in progress.

The James Webb Space Telescope is the world’s premier space science observatory. Webb is solving mysteries in our solar system, looking beyond to distant worlds around other stars, and probing 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.




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Margaret W. Carruthers
Space Telescope Science Institute, Baltimore, Maryland

Christine Pulliam
Space Telescope Science Institute, Baltimore, Maryland

Science: Renyu Hu (NASA-JPL)

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Thursday, May 26, 2022

Geology from 50 Light-Years: Webb Gets Ready to Study Rocky Worlds

Illustration of Exoplanet 55 Cancri e and Its Star
Credits: ARTWORK: NASA, ESA, CSA, Dani Player (STScI)

Illustration of Exoplanet LHS 3844 b and Its Star
Credits: ARTWORK: NASA, ESA, CSA, Dani Player (STScI)

Comparison of Exoplanets 55 Cancri e and LHS 3844 b to Earth and Neptune
Credits: ILLUSTRATION: NASA, ESA, CSA, Dani Player (STScI)

Simulated Thermal Emission Spectrum of Exoplanet LHS 3844 b
Credits: Illustration: NASA, ESA, CSA, Dani Player (STScI)
Science: Laura Kreidberg (MPI-A), Renyu Hu (NASA-JPL)

 


With its mirror segments beautifully aligned and its scientific instruments undergoing calibration, NASA’s James Webb Space Telescope is just weeks away from full operation. Soon after the first observations are revealed this summer, Webb’s in-depth science will begin.

Among the investigations planned for the first year are studies of two hot exoplanets classified as “super-Earths” for their size and rocky composition: the lava-covered 55 Cancri e and the airless LHS 3844 b. Researchers will train Webb’s high-precision spectrographs on these planets with a view to understanding the geologic diversity of planets across the galaxy, and the evolution of rocky planets like Earth.

Super-Hot Super-Earth 55 Cancri e

55 Cancri e orbits less than 1.5 million miles from its Sun-like star (one twenty-fifth of the distance between Mercury and the Sun), completing one circuit in less than 18 hours. With surface temperatures far above the melting point of typical rock-forming minerals, the day side of the planet is thought to be covered in oceans of lava.

Planets that orbit this close to their star are assumed to be tidally locked, with one side facing the star at all times. As a result, the hottest spot on the planet should be the one that faces the star most directly, and the amount of heat coming from the day side should not change much over time.

But this doesn’t seem to be the case. Observations of 55 Cancri e from NASA’s Spitzer Space Telescope suggest that the hottest region is offset from the part that faces the star most directly, while the total amount of heat detected from the day side does vary.

Does 55 Cancri e Have a Thick Atmosphere?

One explanation for these observations is that the planet has a dynamic atmosphere that moves heat around. “55 Cancri e could have a thick atmosphere dominated by oxygen or nitrogen,” explained Renyu Hu of NASA’s Jet Propulsion Laboratory in Southern California, who leads a team that will use Webb’s Near-Infrared Camera (NIRCam) and Mid-Infrared Instrument (MIRI) to capture the thermal emission spectrum of the day side of the planet. “If it has an atmosphere, [Webb] has the sensitivity and wavelength range to detect it and determine what it is made of,” Hu added.

Or Is It Raining Lava in the Evening on 55 Cancri e?

Another intriguing possibility, however, is that 55 Cancri e is not tidally locked. Instead, it may be like Mercury, rotating three times for every two orbits (what’s known as a 3:2 resonance). As a result, the planet would have a day-night cycle.

“That could explain why the hottest part of the planet is shifted,” explained Alexis Brandeker, a researcher from Stockholm University who leads another team studying the planet. “Just like on Earth, it would take time for the surface to heat up. The hottest time of the day would be in the afternoon, not right at noon.”

Brandeker’s team plans to test this hypothesis using NIRCam to measure the heat emitted from the lit side of 55 Cancri e during four different orbits. If the planet has a 3:2 resonance, they will observe each hemisphere twice and should be able to detect any difference between the hemispheres.

In this scenario, the surface would heat up, melt, and even vaporize during the day, forming a very thin atmosphere that Webb could detect. In the evening, the vapor would cool and condense to form droplets of lava that would rain back to the surface, turning solid again as night falls.

Somewhat Cooler Super-Earth LHS 3844 b

While 55 Cancri e will provide insight into the exotic geology of a world covered in lava, LHS 3844 b affords a unique opportunity to analyze the solid rock on an exoplanet surface.

Like 55 Cancri e, LHS 3844 b orbits extremely close to its star, completing one revolution in 11 hours. However, because its star is relatively small and cool, the planet is not hot enough for the surface to be molten. Additionally, Spitzer observations indicate that the planet is very unlikely to have a substantial atmosphere.

What Is the Surface of LHS 3844 b Made of?

While we won’t be able to image the surface of LHS 3844 b directly with Webb, the lack of an obscuring atmosphere makes it possible to study the surface with spectroscopy.

“It turns out that different types of rock have different spectra,” explained Laura Kreidberg at the Max Planck Institute for Astronomy. “You can see with your eyes that granite is lighter in color than basalt. There are similar differences in the infrared light that rocks give off.”

Kreidberg’s team will use MIRI to capture the thermal emission spectrum of the day side of LHS 3844 b, and then compare it to spectra of known rocks, like basalt and granite, to determine its composition. If the planet is volcanically active, the spectrum could also reveal the presence of trace amounts of volcanic gases.

The importance of these observations goes far beyond just two of the more than 5,000 confirmed exoplanets in the galaxy. “They will give us fantastic new perspectives on Earth-like planets in general, helping us learn what the early Earth might have been like when it was hot like these planets are today,” said Kreidberg.

These observations of 55 Cancri e and LHS 3844 b will be conducted as part of Webb’s Cycle 1 General Observers program. General Observers programs were competitively selected using a dual-anonymous review system, the same system used to allocate time on Hubble. The James Webb Space Telescope is the world's premier space science observatory. 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.



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Media Contact:

Margaret W. Carruthers
Space Telescope Science Institute, Baltimore, Maryland

Christine Pulliam
Space Telescope Science Institute, Baltimore, Maryland

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Monday, March 08, 2021

A blazing nearby super-Earth

Artistic impression of the surface of the newly discovered hot super-Earth Gliese 486b. With a temperature of about 700 Kelvin (430 °C), the astronomers of the CARMENES collaboration expect a Venus-like hot and dry landscape interspersed with glowing lava rivers. Gliese 486b possible has a tenuous atmosphere. © Image: RenderArea

The graph illustrates the orbit of a transiting rocky exoplanet like Gliese 486b around its host star. During transit, the planet obscures the stellar disk. Simultaneously, a tiny portion of the starlight passes through the planet’s atmospheric layer. While Gliese 486b continues to orbit, parts of the illuminated hemisphere become visible like lunar phases until the planet vanishes behind the star.  © Image: MPIA graphics department

During the recent two and a half decades, astronomers have discovered thousands of exoplanets made of gas, ice and rock. Only a few of them are Earth-like. However, probing their atmospheres with the currently available instrumentation is challenging at best. Now, astronomers of the CARMENES consortium have published a new study, led by Trifon Trifonov from the Max Planck Institute for Astronomy, which reports the discovery of a hot rocky super-Earth orbiting the nearby red dwarf star Gliese 486. Despite its small separation from the parent star, the planet designated Gliese 486b possibly has retained a part of its original atmosphere. Therefore, Gliese 486b is uniquely suited to examine its atmosphere and interior with the next generation of space-borne and ground-based telescopes. The results are published in the journal Science today.

With the advent of efficient exoplanet-hunting facilities, the numbers of newly discovered worlds outside the Solar System quickly rose to thousands. By combining different observing techniques, astronomers have determined planetary masses, sizes, and even bulk densities, allowing them to estimate their internal composition. The next goal to fully characterize those exoplanets similar to Earth by studying their atmospheres is much more challenging. Especially for rocky planets like Earth, any such atmosphere consists of a thin layer, if it exists at all. As a result, many current atmospheric models of rocky planets remain untested.

Planetary atmospheres must meet specific prerequisites to observe them with next-generation observatories. At a distance of only 26 light-years, scientists of the CARMENES (Calar Alto high-Resolution search for M dwarfs with Exoearths with Near-infrared and optical Échelle Spectrographs) consortium now have found a planet orbiting the red dwarf star Gliese 486 that perfectly satisfies these specifications for rocky planets. The newly discovered planet designated Gliese 486b is a super-Earth with a mass 2.8 times that of our home planet. It is also 30% bigger than Earth. The scientists employed both transit photometry and radial velocity spectroscopy to obtain their results.

The proximity of this exoplanet is exciting because it will be possible to study it in more detail with powerful telescopes such as the upcoming James Webb Space Telescope and the future Extremely Large Telescopes,” Trifon Trifonov explains. He is a planetary scientist at the Max Planck Institute for Astronomy (MPIA) and lead author of the article that features this discovery.

By calculating the planet’s mean density from the mass and radius measurements, its composition appears similar to Venus and Earth, including a metallic core. Anyone standing on Gliese 486b would feel a gravitational pull that is 70% stronger than what we experience on our world.

Gliese 486b revolves around its host star on a circular trajectory within 1.5 days and at a distance of 2.5 million kilometres. One rotation takes the same amount of time, so one side always faces the star. Although the star Gliese 486 is much fainter and cooler than the Sun, the irradiation is so intense that the planet’s surface heats up to at least 700 Kelvin (approx. 430 °C). In this sense, Gliese 486b’s surface probably looks more like Venus than Earth, with a hot and dry landscape interspersed with glowing lava rivers. However, unlike Venus, Gliese 486b possibly only has a tenuous atmosphere if any. Model calculations may be consistent with both scenarios because stellar irradiation tends to evaporate atmospheres. At the same time, the planet’s gravity helps to retain it. Figuring out the balance of those contributions is difficult.

The discovery of Gliese 486b was a stroke of luck. A hundred degrees hotter and the planet’s entire surface would be lava. Its atmosphere would consist of vapourised rocks,” José A. Caballero of the Centro de Astrobiología (CSIC-INTA, Spain) and co-author of the paper concludes. “On the other hand, if Gliese 486b were a hundred degrees colder, it would have been unsuitable for follow-up observations.

The future measurements that the CARMENES team have in mind exploit the orbital orientation, which causes Gliese 486b to cross the surface of the host star from our point of view. Whenever this happens, a tiny fraction of the stellar light shines through the thin atmospheric layer before it reaches Earth. The various compounds absorb light at specific wavelengths, leaving their footprint in the signal. By using spectrographs, the astronomers split up the light according to wavelengths and look for absorption features to derive the atmospheric composition and dynamics. This method is also known as transit spectroscopy.

A second spectroscopic measurement, called emission spectroscopy, is planned when parts of the illuminated hemisphere become visible like lunar phases during Gliese 486b’s orbit until it vanishes behind the star. The spectrum contains information on the bright, hot planetary surface.

We can hardly wait for the new telescopes to become available,” Trifonov admits. “The results will help us to understand how well rocky planets can hold their atmospheres, what they are made of and how they influence the energy distribution on the planets.

Both Trifonov and Caballero collaborate in the CARMENES project, whose consortium comprises eleven research institutions in Spain and Germany. Its purpose is to monitor some 350 red dwarf stars for signs of low-mass planets using a spectrograph mounted at the 3.5 m Calar Alto telescope (Spain). This study includes additional spectroscopic measurements to infer Gliese 486b’s mass. The scientists obtained observations with the MAROON-X instrument at the 8.1 m Gemini North telescope (USA) and retrieved archival data from the 10 m Keck telescope (USA) and the ESO 3.6 m telescope (Chile).

Photometric observations to derive the planet’s size stem from the TESS (Transiting Exoplanet Survey Satellite) spacecraft (NASA, USA), the MuSCAT2 (Multicolour Simultaneous Camera for studying Atmospheres of Transiting exoplanets 2) instrument mounted at the 1.52 m Telescopio Carlos Sánchez at Observatorio del Teide (Spain), and the LCOGT (Las Cumbres Observatory Global Telescope), among others.

Source: Max Planck Institute for Astronomy


Background information

The team was composed of T. Trifonov (Max-Planck-Institut für Astronomie [MPIA]), J. A. Caballero (Centro de Astrobiología [CAB]), J. C. Morales (Institut de Ciències de l'Espai [ICE] and Institut d’Estudis Espacials de Catalunya [IEEC-CSIC]), A. Seifahrt (The University of Chicago), I. Ribas (ICE/IEEC-CSIC), A. Reiners (Institut für Astrophysik, Georg-August-Universität Göttingen [Uni Göttingen]), J. L. Bean (The University of Chicago), R. Luque (Instituto de Astrofísica de Canarias [IAC] and Universidad de La Laguna [ULL]), H. Parviainen (IAC/ULL), E. Pallé (IAC/ULL), S. Stock (Zentrum für Astronomie der Universität Heidelberg [ZAH]) , M. Zechmeister (The University of Chicago), P. J. Amado (Instituto de Astrofísica de Andalucía [IAA-CSIC]), G. Anglada-Escudé (ICE/IEEC-CSIC), M. Azzaro (Centro Astronómico Hispano-Alemán [CAHA]), T. Barclay (NASA Goddard Space Flight Center, and University of Maryland), V. J. S. Béjar (IAC/ULL), P. Bluhm (ZAH), N. Casasayas-Barris (IAC/ULL), C. Cifuentes (CAB), K. A. Collins (Center for Astrophysics, Harvard & Smithsonian [CfA]), K. I. Collins (George Mason University), M. Cortés-Contreras (CAB), J. de Leon (The University of Tokyo), S. Dreizler (Uni Göttingen), C. D. Dressing (University of California at Berkeley), E. Esparza-Borges (IAC/ULL), N. Espinoza (Space Telescope Science Institute), M. Fausnaugh (Massachusetts Institute of Technology [MIT]), A. Fukui (The University of Tokyo), A. P. Hatzes (Thüringer Landessternwarte Tautenburg), C. Hellier (Keele University), Th. Henning (MPIA), C. E. Henze (NASA Ames Research Center), E. Herrero (ICE/IEEC-CSIC), S. V. Jeffers (Uni Göttingen), J. M. Jenkins (NASA Ames Research Center), E. L. N. Jensen (Swarthmore College), A. Kaminski (ZAH), D. Kasper (The University of Chicago), D. Kossakowski (MPIA), M. Kürster (MPIA), M.Lafarga (ICE/IEEC-CSIC), D. W. Latham (CfA), A. W. Mann (University of North Carolina at Chapel Hill,), K. Molaverdikhani (ZAH), D. Montes (Departamento de Física de la Tierra y Astrofísica & IPARCOS-UCM), B. T. Montet (University of New South Wales), F. Murgas (IAC and Departamento de Astrofísica, ULL), N. Narita (The University of Tokyo, Japan Science and Technology Agency, Astrobiology Center, and IAC), M. Oshagh (IAC and Departamento de Astrofísica, ULL), V. M.Passegger (Universität Hamburg and University of Oklahoma,), D. Pollacco (University of Warwick), S. N. Quinn (CfA), A. Quirrenbach (ZAH), G. R. Ricker (MIT), C. Rodríguez López (IAA), J. Sanz-Forcada (CAB), R. P. Schwarz (Patashnick Voorheesville Observatory), A. Schweitzer (Universität Hamburg), S. Seager (MIT), A. Shporer (MIT), M. Stangret (IAC/ULL), J. Stürmer (Universität Heidelberg), T. G. Tan (MIT), P. Tenenbaum (MIT), J. D. Twicken (SETI Institute and NASA Ames Research), R. Vanderspek (MIT), and J. N. Winn (Princeton University).



Contact

Dr. Trifon Trifonov
Phone:+49 6221 528-443 

Dr. Markus Nielbock
span style="color: #f1c232;">Press and public relations officer
Phone:+49 6221 528-134
Max Planck Institute for Astronomy, Heidelberg
Mobile: +49 15678 747326



Original Aplication
 
1. T. Trifonov, J. A. Caballero, J. C. Morales et al.
A nearby transiting rocky exoplanet that is suitable for atmospheric investigation
 



Video  -  A journey to Gliese 486b

This virtual journey to Gliese 486b begins with its position in the night sky. After focusing on the parent star Gliese 486b, the film depicts the measurements. Finally, we fly to the exoplanet Gliese 486b and explore its possible surface, which probably resembles Venus, with a hot and dry landscape interspersed with glowing lava flows. 



Monday, April 11, 2016

Don't come too close to the stars if you are a super-Earth

Artist's impression of a hot super-Earth being stripped of it's atmosphere due to being too close to the mother planet.
Image credit: Peter Devine


Coming too close to the fire will get your fingers burnt. This is also valid for exoplanets orbiting remote stars. Mia S. Lundkvist et al; many affiliated with SAC, have shown that it is also true in the real world. Recent paper titled "Hot super-Earths stripped by their host stars" in Nature Communications.

Coming too close to the fire will get your fingers burnt. This old adage is also valid for exoplanets orbiting remote stars. This is not a big surprise to anyone in the astronomical business, and theoretical calculations have already pointed this out. Now Mia S. Lundkvist and a group of astronomers, of which many are affiliated with the Stellar Astrophysics Centre at Aarhus University, Denmark, have shown that it is also true in the real world.

In the newly published paper titled "Hot super-Earths stripped by their host stars" in Nature Communications the researchers explain their methods and results.

What goes wrong for the super-Earths?

Planets with diameters beetween 2.2 and 3.8 times bigger than the Earth, and orbiting so close to their parent star that they recieve more than 650 times more starlight than what we on Earth recieve from the Sun, will loose their atmospheres due to the intense high energetic radiation from the star. The outer layers of these planets, consisting of a rocky core and a thick atmosphere of gasses, will be heated by the radiation, causing the volatile materials to boil away and disappear into space, leaving the 'naked' planetary cores. It might be compared to being far too close to a hair dryer on full heating power. For the discovery the researchers have been using data from the NASA Kepler mission. Head author Mia S. Lundkvist explains: "The lack of warm planets slightly larger than the Earth, has been suspected for some time. Our results have finally confirmed what theory predicts." Mia adds: "These results are an important step towards understanding how planetary systems evolve. Studying our own Solar system has not helped in this connection. We do not have this type of planets here. Planets Uranus and Neptune are of the right sizes, but they orbit far from the Sun, in much colder regions."


In a diagram like this, with exoplanets placed according to size along the vertical axis and radiation flux along the horizontal axis, the astronomers have discovered a 'desert' where no planets exist. This is the hatched area to the right. 


How do we know?


How close an exoplanet can approach it's star before the volatile constituents boil up and are blown away into space can be calculated from theory.

A missing group of exoplanets in the "exoplanets' zoo" has therefore been expected. The new results from the team of researchers now confirm this, using asteroseismology. In ordinary seismology, geologists study the innards of the Earth using oscillations caused by earthquakes and explosions. Asteroseismology is a bit of the same. A stars is an enormous ball of hot gasses, and it vibrates like a huge bell or a salad bowl of crystal. These vibrations or oscillations can be observed by Kepler, as very small changes in the light output of the star enable the astronomers to 'see' into the star.

Kepler has observed some 2 000 exoplanets, and more are due in the future. The planets are discovered because the cast a small 'shadow' for a few hours while transiting in front of the star, as seen from Earth. By combining measurements of these transits with asteroseismology, the diameter of the planet and the flux, i.e. the total radiation from the star, it receives can be calculated with much higher precision than has previously been possible. Mia S. Lundkvist explains: "We have used asteroseismology as a very good ruler, enabling us to determine the sizes of the exoplanets together with with the flux recieved from their stars."

Confirmation of 'The Desert'

Out of the group of authors, 29 in total most are or have been asociated with the Stellar Astrophysics Centre at Aarhus University, Denmark.

Head author is the young PhD Mia S. Lundkvist, presently working at Zentrum für Astronomie at Heidelberg University, Germany. Mia Lundkvist comments: "For some time we have known that this 'desert' should be there, but now we can see that it is true, after having worked through asteroseismic Kepler data from 102 stars and having calculated 10 million possible scenaria to ensure that what we see here is not only statistical fluctuations. The 'desert' is there, and it is exactly where we expected it to be."

What happens to the stripped planets?

If all the volatiles around a super-Earth have been blown away, what is left? The heavier elements, forming the nucleus of the original planet, will hardly be stripped away by even the strongest stellar radiation, causing the researchers to expect that these 'naked' planetary remnants can be detected and characterized in the future. One of the tools for that will be NASA's TESS mission to be launched in 2017.

link to article www.nature.com/search




Monday, November 02, 2015

Worlds within Worlds: Hubble Peels Back the Layers of a Warm Neptune

Take Neptune for example. For many years, especially since 1989 when Voyager 2 flew past Neptune and measured its gravity field, astronomers have known that the blue giant harbors a secret world inside. Hidden deep below the azure cloud tops lies a rocky core not much larger than Earth. Uranus has one, too! These “worlds within worlds” could have exotic properties including scorching hot oceans and diamond rain.

If only researchers could peel back the clouds for a closer look….

Astronomers using NASA’s Hubble Space Telescope have discovered an immense cloud of hydrogen evaporating from a Neptune-sized planet named GJ 436b. The planet’s atmosphere is evaporating because of extreme irradiation from its parent star. Sciencecast Video


About 30 light years away, a Neptune-sized planetis having some of its layers peeled back.

Astronomers using NASA’s Hubble Space Telescope have discovered an immense cloud of hydrogen evaporating from a Neptune-sized planet named GJ 436b.

“This cloud is spectacular,” says the study’s leader, David Ehrenreich of the Observatory of the University of Geneva in Switzerland. “The research team has nicknamed it ‘The Behemoth.’”

The planet’s atmosphere is evaporating because of extreme irradiation from its parent star—a process that might have been even more intense in the past.

“The parent star, which is a faint red dwarf, was once more active,” says Ehrenreich. “This means that the planet’s atmosphere evaporated faster during its first billion years of existence. Overall, we estimate that the planet may have lost up to 10 percent of its atmosphere.”

GJ 436b is considered to be a “Warm Neptune” because of its size and because it is much closer to its parent star than Neptune is to our own sun. Orbiting at a distance of less than 3 million miles, It whips around the central red dwarf in just 2.6 Earth days. For comparison, the Earth is 93 million miles from the sun and orbits it every 365.24 days.

Systems like GJ 436b could explain the existence of so-called “Hot Super-Earths.”

“Hot Super-Earths” are larger, hotter versions of our own planet. Space telescopes such as NASA’s Kepler and the French led CoRoT have discovered hundredsof them orbiting distant stars. The existence of The Behemoth suggests that Hot Super-Earths could be the remnants of Warm Neptunes that completely lost their gaseous atmospheres to evaporation.

Finding a cloud around GJ 436b required Hubble’s ultraviolet vision. Earth’s atmosphere blocks most ultraviolet light so only a space telescope like Hubble could make the crucial observations.

“You would not see The Behemoth in visible wavelengths because it is optically transparent,” says Ehrenreich. On the other hand, it is opaque to UV rays. “So when you turn the ultraviolet eye of Hubble onto the system, it’s really kind of a transformation because the planet turns into a monstrous thing.”

The ultraviolet technique could be a game-changer in exoplanet studies, he adds. Ehrenreich expects that astronomers will find thousands of Warm Neptunes and Super-Earths in the years ahead. 

Astronomers will want to examine them for evidence of evaporation. Moreover, the ultraviolet technique might be able to spot the signature of oceans evaporating on Earth-like planets, shedding new light on worlds akin to our own.

Maybe you can’t judge a book by its cover, but you can judge a planet by its Behemoth.