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An observational signature of evolved oceans on extra-solar terrestrial planets
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AN OBSERVATIONAL SIGNATURE OF EVOLVED OCEANS
ON EXTRA-SOLAR TERRESTRIAL PLANETS
M. Jura
Department of Physics and Astronomy, University of California, Los Angeles CA
90095-1562; jura@clotho.astro.ucla.edu
ABSTRACT
The increase in luminosity with time of a main sequence star eventually can
lead to substantial evaporation of the oceans on an orbiting terrestrial planet.
Subsequently, the gas-phase H2O in the planet’s upper atmosphere can be pho-
todissociated by stellar ultraviolet and the resulting atomic hydrogen then may
be lost in a wind. This gaseous envelope may pass in front of the host star
and produce transient, detectable ultraviolet absorption in the Lyman lines in
systems older than 1 Gyr.
Subject headings: astrobiology – (stars): planetary systems
1. INTRODUCTION
The possible existence of life on other planets is of central interest in modern astronomy.
A standard working hypothesis is that liquid water is required for life, and here we describe
an observational signature of evolved oceans on extra-solar terrestrial planets.
The occultation of HD 209458 by a Jovian planet has demonstrated that it is possible
to study the atmospheres of extra-solar planets with absorption line spectroscopy during a
transit (Charbonneau et al. 2000, 2002). The Lyman α spectrum of HD 209458 observed
during its companion planet’s transit can be explained as an outflow of hydrogen from this
planet (Vidal-Madjar et al. 2003. Liang et al. 2003) that also has entrained other gases
(Vidal-Madjar et al. 2004). Below, we describe an extension of this technique to study
gaseous winds from terrestrial planets.
To date, only Jovian mass extra-solar planets have been detected. The discovery of
terrestrial planets by occultations of their host stars is the goal of future space missions such
as Kepler (see, for example, Jenkins 2002). In addition to transits discovered by photometry,
it may be possible to perform trans
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