Issue |
A&A
Volume 439, Number 2, August IV 2005
|
|
---|---|---|
Page(s) | 771 - 775 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361:20052946 | |
Published online | 29 July 2005 |
Roche lobe effects on expanded upper atmospheres of short-periodic giant exoplanets
1
Institute for Geophysics, Astrophysics, and Meteorology, University of Graz, Universitätsplatz 5, 8010 Graz, Austria e-mail: gerald.jaritz@stud.uni-graz.at
2
Space Research Institute, Austrian Academy of Sciences, Schmiedlstrasse 6, 8042 Graz, Austria e-mail: [helfried.biernat;helmut.lammer;daniel.langmayr]@oeaw.ac.at
3
Institute for Theoretical Physics, University of Graz, Universitätsplatz 5, 8010 Graz, Austria e-mail: stefan.endler@stud.uni-graz.at
4
Institut für Theoretische Physik, Technische Universität Braunschweig, Mendelssohnstrasse 3, 38106 Braunschweig, Germany e-mail: j-m.griessmeier@tu-bs.de
5
Institute for Computational Modelling, Russian Academy of Sciences, Krasnoyarsk 36, Russian Federation e-mail: erkaev@icm.krasn.ru
Received:
13
December
2004
Accepted:
2
May
2005
Theoretical studies and recent observational evidence of
the expansion of the atmospheres of short-periodic exoplanets show
that the atmospheres extend up to several planetary radii. This
indicates that the atmospheres experience blow-off conditions.
Because of the short orbital distance to their host stars, the
expansion of the upper atmosphere is no longer radially symmetric,
but depends on the direction to the central body, resulting in a
deformation of the expanded atmosphere. We show the connection
between atmospheric expansion, tidal forces and effects of the
Roche potential and find that HD 209458 b, OGLE-TR-10 b and
OGLE-TR-111 b are most likely in a state of classical
hydrodynamical blow-off, because the distance where blow-off can
occur is less than the distance to the Lagrangian point L1. On the
other hand, OGLE-TR-56 b, OGLE-TR-113 b, OGLE-TR-132 b and TreS-1 experience a geometrical blow-off defined by the Roche lobe as proposed by Lecavelier des Etangs et al. (2004, A&A, 418, L1). Our results have important implications for the evolution of short periodic gas giants,
because the Roche lobe overflow of the atmosphere can lead to
lower mass loss rates over the exoplanets history, compared to gas
giants which experience hydrodynamic expansion and loss unaffected
by this boundary. Thus, massive exoplanets like OGLE-TR-56 b in
very close orbital distances are subject to geometrical blow-off
conditions, this results in a total mass loss for this particular
exoplanet of the order of about 3 10-2 Mpl over
the planets age, even if current mass loss rates of about 2
1011 g s-1 are calculated. If the exoplanet effected by the geometrical blow-off is more massive, the mass loss rate is even lower. However, giant exoplanets like HD 209458 b, OGLE-TR-10 b and OGLE-TR-111 b at orbital distances of about 0.05 AU may experience classical hydrodynamic blow-off conditions, which can result in higher mass loss rates. Thus, such planets may shrink to
their core sizes during the X-ray and EUV active periods of their
host stars as proposed by Lammer et al. (2003, ApJ, L121, 598) and Baraffe et al. (2004, A&A, 419, L13).
Key words: radiation mechanisms: non-thermal / acceleration of particles / plasmas / turbulence / gamma rays: theory / methods: analytical
© ESO, 2005
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