The EChO science case
Artikel i vetenskaplig tidskrift, 2015

The discovery of almost two thousand exoplanets has revealed an unexpectedly diverse planet population. We see gas giants in few-day orbits, whole multi-planet systems within the orbit of Mercury, and new populations of planets with masses between that of the Earth and Neptune—all unknown in the Solar System. Observations to date have shown that our Solar System is certainly not representative of the general population of planets in our Milky Way. The key science questions that urgently need addressing are therefore: What are exoplanets made of? Why are planets as they are? How do planetary systems work and what causes the exceptional diversity observed as compared to the Solar System? The EChO (Exoplanet Characterisation Observatory) space mission was conceived to take up the challenge to explain this diversity in terms of formation, evolution, internal structure and planet and atmospheric composition. This requires in-depth spectroscopic knowledge of the atmospheres of a large and well-defined planet sample for which precise physical, chemical and dynamical information can be obtained. In order to fulfil this ambitious scientific program, EChO was designed as a dedicated survey mission for transit and eclipse spectroscopy capable of observing a large, diverse and well-defined planet sample within its 4-year mission lifetime. The transit and eclipse spectroscopy method, whereby the signal from the star and planet are differentiated using knowledge of the planetary ephemerides, allows us to measure atmospheric signals from the planet at levels of at least 10−4 relative to the star. This can only be achieved in conjunction with a carefully designed stable payload and satellite platform. It is also necessary to provide broad instantaneous wavelength coverage to detect as many molecular species as possible, to probe the thermal structure of the planetary atmospheres and to correct for the contaminating effects of the stellar photosphere. This requires wavelength coverage of at least 0.55 to 11 μm with a goal of covering from 0.4 to 16 μm. Only modest spectral resolving power is needed, with R ~ 300 for wavelengths less than 5 μm and R ~ 30 for wavelengths greater than this. The transit spectroscopy technique means that no spatial resolution is required. A telescope collecting area of about 1 m2 is sufficiently large to achieve the necessary spectro-photometric precision: for the Phase A study a 1.13 m2 telescope, diffraction limited at 3 μm has been adopted. Placing the satellite at L2 provides a cold and stable thermal environment as well as a large field of regard to allow efficient time-critical observation of targets randomly distributed over the sky. EChO has been conceived to achieve a single goal: exoplanet spectroscopy. The spectral coverage and signal-to-noise to be achieved by EChO, thanks to its high stability and dedicated design, would be a game changer by allowing atmospheric composition to be measured with unparalleled exactness: at least a factor 10 more precise and a factor 10 to 1000 more accurate than current observations. This would enable the detection of molecular abundances three orders of magnitude lower than currently possible and a fourfold increase from the handful of molecules detected to date. Combining these data with estimates of planetary bulk compositions from accurate measurements of their radii and masses would allow degeneracies associated with planetary interior modelling to be broken, giving unique insight into the interior structure and elemental abundances of these alien worlds. EChO would allow scientists to study exoplanets both as a population and as individuals. The mission can target super-Earths, Neptune-like, and Jupiter-like planets, in the very hot to temperate zones (planet temperatures of 300–3000 K) of F to M-type host stars. The EChO core science would be delivered by a three-tier survey. The EChO Chemical Census: This is a broad survey of a few-hundred exoplanets, which allows us to explore the spectroscopic and chemical diversity of the exoplanet population as a whole. The EChO Origin: This is a deep survey of a subsample of tens of exoplanets for which significantly higher signal to noise and spectral resolution spectra can be obtained to explain the origin of the exoplanet diversity (such as formation mechanisms, chemical processes, atmospheric escape). The EChO Rosetta Stones: This is an ultra-high accuracy survey targeting a subsample of select exoplanets. These will be the bright “benchmark” cases for which a large number of measurements would be taken to explore temporal variations, and to obtain two and three dimensional spatial information on the atmospheric conditions through eclipse-mapping techniques. [...]

IR astronomy

Spectroscopy

Exoplanets

Atmospheric science

Space missions

Författare

G. Tinetti

University College London (UCL)

P. Drossart

Observatoire de Paris-Meudon

P. Eccleston

STFC Rutherford Appleton Laboratory

P. Hartogh

Max-Planck-Gesellschaft

K. Isaak

European Space Research and Technology Centre (ESA ESTEC)

M. Linder

European Space Research and Technology Centre (ESA ESTEC)

C. Lovis

Université de Genève

G. Micela

Istituto nazionale di astrofisica (INAF)

M. Ollivier

Institut d'Astrophysique Spatiale

Observatoire de Paris-Meudon

L. Puig

European Space Research and Technology Centre (ESA ESTEC)

I. Ribas

Institut d'Estudis Espacials de Catalunya (IEEC)

I. Snellen

Universiteit Leiden

B. Swinyard

University College London (UCL)

STFC Rutherford Appleton Laboratory

F. Allard

École Normale Supérieure de Lyon

J. Barstow

University of Oxford

J. Cho

Queen Mary University of London

A. Coustenis

Observatoire de Paris-Meudon

C. Cockell

Royal Observatory

A. Correia

Universidade de Aveiro

L. Decin

KU Leuven

R. J. De Kok

Netherlands Institute for Space Research (SRON)

P. Deroo

Jet Propulsion Laboratory, California Institute of Technology

T. Encrenaz

Observatoire de Paris-Meudon

F. Forget

LMD

A. Glasse

STFC UK-ATC

C. Griffith

University of Arizona

T. Guillot

Observatoire de la Cote d'Azur

T. Koskinen

University of Arizona

H. Lammer

IWF

J. Leconte

LMD

University of Toronto

P. Maxted

Keele University

I. Mueller-Wodarg

Imperial College London

R. Nelson

Queen Mary University of London

C. North

Cardiff University

E. Palle

Instituto de Astrofísica de Canarias

I. Pagano

Istituto nazionale di astrofisica (INAF)

G. Piccioni

Istituto nazionale di astrofisica (INAF)

D. Pinfield

University of Hertfordshire

F. Selsis

Université de Bordeaux

A. Sozzetti

Istituto nazionale di astrofisica (INAF)

L. Stixrude

University College London (UCL)

J. Tennyson

University College London (UCL)

D. Turrini

Istituto nazionale di astrofisica (INAF)

M. Zapatero-Osorio

CAB

J.P. Beaulieu

Institut d 'Astrophysique de Paris

D. Grodent

Universite de Liège

M. Guedel

Universität Wien

D. Luz

Universidade de Lisboa

H. U. Norgaard-Nielsen

DSRI

T. P. Ray

Dublin Institute for Advanced Studies

H. Rickman

Polish Academy of Sciences

Uppsala universitet

A. Selig

Netherlands Institute for Space Research (SRON)

M. Swain

Jet Propulsion Laboratory, California Institute of Technology

M. Banaszkiewicz

Polish Academy of Sciences

M. Barlow

University College London (UCL)

G. Branduardi-Raymont

University of Oxford

V. C. du Foresto

Observatoire de Paris-Meudon

L. Gizon

Universite de Liège

A. Hornstrup

Max-Planck-Gesellschaft

C. Jarchow

Magyar Tudomanyos Akademia

F. Kerschbaum

Max-Planck-Gesellschaft

G. Kovacs

Universität Wien

P.O. Lagage

Magyar Tudomanyos Akademia

T. Lim

Le Commissariat à l’Énergie Atomique et aux Énergies Alternatives (CEA)

T. L. Lim

STFC Rutherford Appleton Laboratory

G. Malaguti

Institut d'Estudis Espacials de Catalunya (IEEC)

E. Pace

Istituto nazionale di astrofisica (INAF)

E. Pascale

Universita degli Studi di Firenze

B. Vandenbussche

Cardiff University

G. Wright

KU Leuven

G.R. Zapata

STFC UK-ATC

R. Azzollini

Istituto nazionale di astrofisica (INAF)

R. Burston

STFC UK-ATC

J. Colomé

Max-Planck-Gesellschaft

M. Crook

Institut d'Estudis Espacials de Catalunya (IEEC)

A. di Giorgio

STFC Rutherford Appleton Laboratory

A. M. di Giorgio

Istituto nazionale di astrofisica (INAF)

R. Hoogeveen

Cardiff University

K. Middleton

STFC Rutherford Appleton Laboratory

G. Morgante

STFC Rutherford Appleton Laboratory

F. Pinsard

Istituto nazionale di astrofisica (INAF)

R. Ottensamer

Universität Wien

M. Rataj

Le Commissariat à l’Énergie Atomique et aux Énergies Alternatives (CEA)

J.M. Reess

Polish Academy of Sciences

G. Savini

Observatoire de Paris-Meudon

Kay Justtanont

Chalmers, Rymd- och geovetenskap, Onsala rymdobservatorium

J.R. Schrader

Netherlands Institute for Space Research (SRON)

R. Stamper

STFC Rutherford Appleton Laboratory

B. Winter

University College London (UCL)

L. Abe

Observatoire de la Cote d'Azur

M. Abreu

Universidade de Lisboa

Experimental Astronomy

0922-6435 (ISSN) 1572-9508 (eISSN)

Vol. 40 2-3 329-391

Ämneskategorier

Fysik

DOI

10.1007/s10686-015-9484-8

Mer information

Senast uppdaterat

2023-09-15