[1] Exoplanet characterisation involves investigating the physical properties (such as radius) and chemical properties (such as atmospheric composition) of an exoplanet. It is crucial both for better understanding planet formation and evolution, and for determining whether complex processes — such as the evolution and maintenance of life — could be possible on an exoplanet.
[2] H– is a negative hydrogen ion that has been formed by the dissociation of a molecule such as H2 (hydrogen) or H2O (water). These molecules dissociate at very high temperatures (over 2500 Kelvins, or 2227 °C).
[3] In astronomy, a ‘metal’ is defined as any element with more protons in its nucleus than hydrogen or helium (which have one and two protons respectively). Thus, ‘metallicity’ is a measure of how many elements or molecules are present that are not hydrogen or helium.
[4] Hot Jupiters are an informal class of exoplanets with short-period orbits (orbiting their parent star in roughly ten days or less), and large, inflated gassy atmospheres. They are of particular interest because i) they are relatively easy to detect and ii) there is no hot Jupiter within our Solar System, so we have to look to exoplanets to study them.
[5] Archival data are data that the team did not collect specifically for this research, but were collected by another team(s) for a different initial purpose and are now publicly available. The reanalysis and repurposing of archival data can be an extremely cost and environmentally effective way of getting new results.
[6] A thermal inversion is a natural phenomenon where a planet’s or exoplanet’s atmosphere does not steadily cool with increased altitude, but instead reverses from cooling to heating at a higher altitude. Thermal inversions are thought to occur because of the presence of certain metallic species in the atmosphere. For example, the Earth’s atmosphere has a thermal inversion that is due to the presence of ozone (O3).
[2] H– is a negative hydrogen ion that has been formed by the dissociation of a molecule such as H2 (hydrogen) or H2O (water). These molecules dissociate at very high temperatures (over 2500 Kelvins, or 2227 °C).
[3] In astronomy, a ‘metal’ is defined as any element with more protons in its nucleus than hydrogen or helium (which have one and two protons respectively). Thus, ‘metallicity’ is a measure of how many elements or molecules are present that are not hydrogen or helium.
[4] Hot Jupiters are an informal class of exoplanets with short-period orbits (orbiting their parent star in roughly ten days or less), and large, inflated gassy atmospheres. They are of particular interest because i) they are relatively easy to detect and ii) there is no hot Jupiter within our Solar System, so we have to look to exoplanets to study them.
[5] Archival data are data that the team did not collect specifically for this research, but were collected by another team(s) for a different initial purpose and are now publicly available. The reanalysis and repurposing of archival data can be an extremely cost and environmentally effective way of getting new results.
[6] A thermal inversion is a natural phenomenon where a planet’s or exoplanet’s atmosphere does not steadily cool with increased altitude, but instead reverses from cooling to heating at a higher altitude. Thermal inversions are thought to occur because of the presence of certain metallic species in the atmosphere. For example, the Earth’s atmosphere has a thermal inversion that is due to the presence of ozone (O3).
More Information
The Hubble Space Telescope is a project of international cooperation between ESA and NASA.
These results have been published in the Astrophysical Journal Supplement Series.
The international team of astronomers in this study consists of: Q. Changeat (University College London, United Kingdom [UCL]), B. Edwards (UCL and Commissariat à l'énergie atomique et aux énergies alternatives [CEA], Université Paris-Saclay, Université de Paris, France), A. F. Al-Refaie (UCL), A. Tsiaras (UCL and Osservatorio Astrofisico di Arcetri, Firenze, Italy), J. W. Skinner (Queen Mary University of London, United Kingdom), J. Y-K. Cho (Center for Computational Astrophysics, Flatiron Institute, New York, USA), K. H. Yip (UCL), L. Anisman (UCL), M. Ikoma (National Astronomical Observatory of Japan, Tokyo, Japan and The Graduate University for Advanced Studies [SOKENDAI], Tokyo, Japan), M. F. Bieger (University of Exeter, United Kingdom), O. Venot (Université de Paris and Université Paris Est Creteil, France), S. Shibata (University of Zurich, Switzerland), I. P. Waldmann (UCL), G. Tinetti (UCL).
Image credit: ESA/Hubble, N. Bartmann
Links
Contacts
Quentin Changeat
University College London
United Kingdom
Email: quentin.changeat.18@ucl.ac.uk
Bethany Downer
ESA/Hubble Chief Science Communications Officer
Email: Bethany.Downer@esahubble.org