Issue |
A&A
Volume 514, May 2010
|
|
---|---|---|
Article Number | A72 | |
Number of page(s) | 10 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/200913347 | |
Published online | 21 May 2010 |
Evaporation of the planet HD 189733b observed in H I Lyman-
A. Lecavelier des Etangs1,2 - D. Ehrenreich3 - A. Vidal-Madjar1,2 - G. E. Ballester4 - J.-M. Désert1,2 - R. Ferlet1,2 - G. Hébrard1,2 - D. K. Sing1,2,5 - K.-O. Tchakoumegni1,2,6 - S. Udry7
1 - CNRS, UMR 7095,
Institut d'astrophysique de Paris,
98bis boulevard Arago, 75014 Paris, France
2 -
UPMC Univ. Paris 6, UMR 7095,
Institut d'Astrophysique de Paris,
98bis boulevard Arago, 75014 Paris, France
3 -
Université Joseph Fourier-Grenoble 1/CNRS,
Laboratoire d'astrophysique de Grenoble (LAOG) UMR 5571,
BP 53, 38041 Grenoble Cedex 09, France
4 -
Lunar and Planetary Laboratory, University of Arizona, 1541 E. University Blvd., Tucson, AZ 85721-0063, USA
5 -
Astrophysics Group, School of Physics, University of Exeter, Stocker Road, Exeter EX4 4QL, UK
6 -
Lycée Passy Buzenval, 50 avenue Otis Mygatt, 92508 Rueil-Malmaison Cedex, France
7 -
Observatoire de Genève, Université de Genève, 51 chemin des Maillettes, 1290 Sauverny, Switzerland
Received 24 September 2009 / Accepted 8 February 2010
Abstract
We observed three transits of the extrasolar planet HD 189733b in H I Lyman-
and in a few other lines in the ultraviolet with HST/ACS, in the search for atmospheric signatures.
We detect a transit signature in the Lyman-
light curve
with a transit depth of
%.
This depth exceeds the occultation depth produced by the planetary disk alone at the 3.5
level (statistical).
Other stellar emission lines are less bright, and, taken individually,
they do not show the transit signature, while the whole spectra redward
of the Lyman-
line has enough photons to show a transit signature consistent with the absorption by the planetary disk alone.
The transit depth's upper limits in the emission lines are 11.1% for O I
1305 Å and 5.5% for C II
1335 Å lines.
The presence of an extended exosphere of atomic hydrogen around HD 189733b producing 5% absorption
of the full unresolved Lyman-
line flux shows that the
planet is losing gas. The Lyman-
light curve
is well-fitted by a numerical simulation
of escaping hydrogen in which the planetary atoms are pushed
by the stellar radiation pressure.
We constrain the escape rate of atomic hydrogen to be between
109 and 1011 g s-1 and the ionizing extreme UV flux
between 2 and 40 times the solar value (1-
),
with higher escape rates corresponding to larger EUV flux.
The best fit is obtained for
g s-1 and
an EUV flux
times the solar value.
HD 189733b is the second extrasolar planet for which atmospheric
evaporation has been detected.
Key words: planetary systems - stars: individual: HD 189733
1 Introduction
1.1 Evaporation of hot Jupiters
Observations of the extrasolar planet HD 209458b in the Lyman-
line
of atomic hydrogen (H I)
have revealed that this planet is losing gas (Vidal-Madjar et al. 2003).
Indeed, since the discovery of 51 Peg b (Mayor & Queloz 1995),
the issue of the evaporation of hot Jupiters (also named ``Pegasides'', Guillot et al. 1996)
has been raised by Burrows & Lunine (1995) and Guillot et al. (1996).
Nonetheless, the discovery of a large number of massive
hot Jupiters
and
very hot Jupiters
has led to the conclusion that the evaporation of massive planets has to be modest.
In this frame the discovery that the transiting extrasolar planet HD 209458b is indeed losing
mass was rather unexpected.
Lyman-
observations of the planetary transit showed excess absorption
due to an extended H I cloud and provided a lower limit of the H I escape rate
on the order of 1010 g s-1 (Vidal-Madjar et al. 2003;
Vidal-Madjar & Lecavelier des Etangs 2004).
This discovery has been challenged by Ben-Jaffel (2007),
but the apparent discrepancy has been resolved and the result obtained
by Ben-Jaffel on this first data set
strengthens the evaporation scenario (Vidal-Madjar et al. 2008).
Two subsequent observations at low spectral resolution
confirm the evaporation with the detection of a 5% absorption
of the whole Lyman-
line, as measured using unresolved emission line flux during
planetary transits observed with the Hubble Space Telescope (HST) STIS
(Vidal-Madjar et al. 2004) and ACS instruments (Ehrenreich et al. 2010).
An independent, new analysis of the low-resolution data set
used by Vidal-Madjar et al. (2004) has confirmed that the transit depth
in Lyman-
is significantly greater than the transit depth due to
the planetary disk alone (Ben-Jaffel & Sona Hosseini 2010).
All of these three independent observations show
a significant amount of gas at velocities exceeding the planet escape velocity,
leading to the conclusion that HD 209458b is evaporating.
Table 1: Log of the observations. Time is given in UT.
These observational constraints have been used to develop several theoretical models to explain and characterize the evaporation processes (Lammer et al. 2003; Lecavelier des Etangs et al. 2004, 2007, 2008a; Baraffe et al. 2004, 2005, 2006; Yelle 2004, 2006; Jaritz et al. 2005; Tian et al. 2005; García-Muñoz 2007; Holmström et al. 2008; Stone & Proga 2009; Murray-Clay et al. 2009). Except for the model of Holmström et al. (2008) in which the observed hydrogen originates from charge exchange between a stellar wind of exotic properties and the planetary escaping exosphere (in this model the escape is found to be of the same order of magnitude), all of these modeling efforts have led to the conclusion that most of the EUV and X-ray energy input by the host star is used by the atmosphere to escape the planetary gravitational potential. Therefore, an ``energy diagram'' has been developed to describe the evaporation status of extrasolar planets, a diagram in which the potential energy of the planet is plotted versus the energy received by its upper atmosphere (Lecavelier des Etangs 2007). It has also been suggested that, in the case of planets with a mass of only a fraction of the mass of a hot Jupiter and orbiting close to their parent stars, evaporation can lead to significant modification of the nature of the planet, leading to the formation of planetary remnants (Lecavelier des Etangs et al. 2004). The recently discovered CoRoT-7b (Léger et al. 2009) could belong to a new category of planets, which was proposed for classification as ``chthonian planets'' (see Lecavelier des Etangs et al. 2004). A review of the evaporation of hot Jupiters can be found in Ehrenreich (2010).
However, up to now HD 209458b has remained the
only planet for which an evaporation process has been observed.
This raises the question of the
evaporation state of other hot Jupiters and very hot Jupiters.
Is the evaporation specific to HD 209458b or general to hot Jupiters?
How does the escape rate depend on the planetary system and stellar characteristics?
The discovery of HD 189733b, a planet transiting a bright and nearby K0 star (V=7.7), offers the
unprecedented opportunity to answer these questions. Indeed, among the stars harboring transiting planets,
HD 189733 belongs to the brightest at Lyman-;
therefore,
despite the failure of the HST/STIS instrument one year before the discovery of HD 189733b,
this planet remained one of the best targets when searching for atmospheric escape.
In this paper we present transit observations of HD 189733b made with the UV channel of
the Advanced Camera for Surveys onboard the Hubble Space Telescope (HST/ACS) using
the same methodology as employed by Ehrenreich et al. (2010) for HD 209458b.
1.2 HD 189733b
Located just 19.3 parsecs away with a semi-major axis of 0.03 AU and an orbital period of 2.2 days, HD 189733b belongs to the class of ``very hot Jupiters'' (Bouchy et al. 2005). More important, since this planet is seen to transit its parent star, the planetary transits and eclipses can be used to probe the planet's atmosphere and environment (e.g., Charbonneau et al. 2008; Désert et al. 2009).
HD 189733b orbits a bright main-sequence star and shows a
transit occultation depth of 2.4% at optical wavelengths
(Pont et al. 2007). The
planet has a mass
Jupiter masses (
)
and a
radius
Jupiter radii (
)
in the visible (Bakos
et al. 2006; Winn et al. 2007). The short period of the planet
(2.21858 days) has been measured precisely (Hébrard & Lecavelier des Etangs 2006; Knutson et al. 2009).
Spectropolarimetry has measured the strength and topology
of the stellar magnetic field, which reaches up to 40 G (Moutou et al. 2007).
Sodium has been detected in the planet's atmosphere
by ground-based observations (Redfield et al. 2008).
Using HST/ACS, Pont et al. (2008) detected atmospheric haze,
which is interpreted as Mie
scattering by small particles (Lecavelier des Etangs et al. 2008b).
High signal-to-noise HST/NICMOS observations (Sing et al. 2009)
have recently shown that the near-IR spectrum below 2
m is
dominated by haze scattering rather than by water absorption (Swain et al. 2008).
It has been tentatively proposed that CO molecules can explain the excess
absorption seen at 4.5
m (Charbonneau et al. 2008; Désert et al. 2009).
Using Spitzer spectroscopy of planetary eclipses, the infrared spectra
of HD 189733b's atmosphere have revealed signatures of H2O absorption
and possibly weather-like variations in the atmospheric conditions
(Grillmair et al. 2008). A sensitive search with GMRT has
provided very low upper limits on the meter-wavelength radio emission from the planet,
indicating a weak planetary magnetic field (Lecavelier des Etangs et al. 2009).
2 Observations
Using the slitless prism spectroscopy mode of the Solar Blind Camera (SBC) of the
HST/ACS, we observed 3 transits of HD 189733b.
These observations provide 2D spectral images covering the far-UV
wavelengths from 1200 Å to
1700 Å.
The log of the observations is given in Table 1.
We observed during four HST orbits for the first two transits,
and during three HST orbits for the last transit.
For each series of exposures within a given HST orbit,
we obtained four individual exposures with the target at a first position on the detector,
and four other exposures at a second position (dithering).
We thus obtained a total of 32 exposures for transits #1 and #2
and 24 exposures for transit #3.
Each exposure had 257 s effective exposure time.
3 Data analysis
![]() |
Figure 1: 2D image of the HD 189733 spectrum obtained with ACS prism spectroscopy ( upper panel). The bottom panel shows the 2D-model of this image. In this image, stellar emission lines can be seen as bright spots: from left to right, the six brightest spots are the Lyman-alpha line, followed by the two O I and C II emission features, further to the right is the Si IV feature, and the two last spots are emission by C IV and C I. The stellar continuum emission is seen as a horizontal bright line along the spectrum. |
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The data consist of 2D prism dispersed images of the star HD 189733.
At these far-UV wavelengths, the spectrum of a K-type star is composed
of well-known bright chromospheric emission lines arising
above a faint photospheric continuum. These emission lines form features
that are seen as bright spots in the 2D images (Fig. 1).
The brightest line is the H I Lyman-
at
1216 Å.
By identifying other features (e.g., H I, O I, C II, etc.)
the spectrum can be wavelength-calibrated.
The aim of the data analysis is to obtain the best estimate of the brightness
of each emission feature (with its associated error bar)
in order to search for a possible transit signature.
The first step is to subtract the background of each image.
This background is caused mainly by the bright geocoronal Lyman-
airglow that
produces a roughly uniform background entering the detector in the slitless prism mode.
This background is accurately determined by the mean flux measured in each image
above and below the stellar spectrum.
We used two wide zones 100 pixels high centered 100 pixels above and below the spectrum.
The background level is found to vary significantly within a given HST orbit.
Nonetheless, various tests show that the background estimate is robust and its associated error
is negligible in the final error budget, well below the photon noise of all the measured
emission features.
To estimate the brightness of each emission feature,
we fitted each 2D spectral image with a
parametric model and calculated the total number of counts in each line after
subtracting the modeled 2D flux from the other emission features and from the continuum.
For each 2D spectral image, the fit to the image was performed in 3 steps.
First, we calculated a preliminary point spread function (PSF)
by fitting the Lyman-
emission line.
In the second step, the whole image was fitted with a model of six emission features whose
positions were free to vary. In this fit, the initial guess for the features positions
was set close to the six brightest spots as seen in Fig. 1
(H I, O I, C II, Si IV, C IV, C I).
This second step was used to obtain a preliminary
wavelength calibration by using the brightest emission lines.
Finally, in a third step,
we performed a fit of the whole 2D image in which the list of emission lines was extended to fainter lines.
In this final stage the model included
the wavelengths of the emission lines as a fixed parameter, while the wavelength
calibration was free to vary and
was defined by a 3rd order polynomial in the X direction and a 1st order
polynomial in the Y direction. The line list input to the model
was defined by trial and error; few misidentifications at the beginning of
the process were easily corrected (even for faint lines) by checking the lines
positions on a wavelength calibration plot. We ended
up with a line list given in Table 2.
Table 2: List of lines used to fit the 2D images.
The intrinsic width of the observed emission lines
is much smaller than the prism resolution, so the
lines can be used to estimate the instrumental
PSF.
In all three steps of the fitting procedure,
the PSF was modeled by the addition of six Gaussians.
The sharpest Gaussian is an asymmetrical 2D Gaussian whose widths
along the two axes and the orientation are free to vary.
This sharp Gaussian has a width of about one pixel, and
was found to vary from one exposure to the next;
this is likely
due to the telescope jitter.
The five other Gaussians are axi-symmetrical Gaussians of fixed widths :
pixels,
pixels,
pixels,
pixels, and
pixels.
These widths had been obtained by numerous experiments and allowed us to obtain the best fit to the data.
The stellar continuum was found to be well-fitted by an exponential law in the form
,
where a and b are free parameters.
This stellar continuum model was also convolved with
the PSF defined in the previous paragraph.
The resulting wavelength calibration (third degree polynomial)
is plotted in Fig. 2 together with the
features positions obtained at the second step of the fit. It is clear that the
3rd degree polynomial gives a satisfactory wavelength calibration.
This calibration also allow correction for misidentifications.
For instance, we first believed that the line between the N V doublet and the O I emission
feature was a line of Si II from the ground level at 1260.4 Å.
But its measured position was significantly off
the wavelength calibration. We thus realized that this
line is in fact a line of Si II* at
1264.7 Å, the Si II line being
extincted by the interstellar medium absorption.
To obtain the wavelength calibrated spectrum of HD 189733 plotted in Fig. 3,
![]() |
Figure 2: Plot of the wavelength calibration. The squares show the position of each identified emission feature as a function of wavelength. The solid line shows the fit by a third-degree polynomial. |
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![]() |
Figure 3: Plot of one-dimensional wavelength calibrated ACS spectrum of HD 189733. The brightest lines are identified. |
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With the PSF parameters (8 parameters), the wavelength calibration (6 parameters), the brightness of each line (10 parameters for a total of 10 lines), the stellar continuum (2 parameters), and a free parameter to fit the residual background assumed to be constant within the image (1 parameter), each image is fitted with a total of 27 parameters.
Finally, after obtaining the best fit to each individual 2D image, we calculated a model image for each line using the best fit parameters, but changing the brightness parameter of the measured line to zero. This model image is subtracted from the data image, providing the best estimate of the line image in which the contribution of all other lines and of the continuum has been removed. We measured the brightness in the line image using aperture photometry. The error bars were calculated using the 2D image of the propagated errors provided by the instrument pipeline; these errors are mainly dominated by the photon noise. The resulting brightnesses were used to obtain the transit light curves plotted and discussed in Sect. 4.
4 Transit light curves
4.1 H I Lyman-
light curve
![]() |
Figure 4:
Lyman- |
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![]() |
Figure 5:
Flux of the Lyman- |
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![]() |
Figure 6: Same as previous plot in which the data have been rebinned by four. The possible difference of transit depth between different epochs are visible here. |
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Table 3:
Results from the Lyman-
light curve.
The main objective of these observations is to obtain the transit light curve
in H I Lyman-
and to search for an atmospheric evaporation signature.
For each of the three transits, we plotted the resulting light curves
(Fig. 4). We fitted each light curve
as a function of time by a transit model defined by a linear baseline
for the stellar Lyman-
flux and the occultation
by an optically-thick disk with the planetary ephemerides.
The results from these three independent fits are given in Table 3.
We see that the second transit gives noisier measurements than the first one, and the observations were made only when the planet was off transit or during the partial occultation phase. In this transit #2, no measurements during the total phase of the planetary transit were obtained because of the Earth occultation of the target as seen by HST. In the first and third transits, the data covered all phases of the transit light curve, and measurements well before and after the transit allowed for estimates of the light curve baseline. Measurements obtained during the total phase of the planetary transit are well-fitted by a transit light curve of an optically-thick occulting disk (Fig. 4), providing an estimate of the size of the H I occulting cloud.
The full set of Lyman-
measurements can be
phase-folded to provide a complete transit
light curve (Figs. 5 and 6).
The dispersion of the data rebinned by four is roughly divided by two,
so there is no sign of red-noise in the data.
The fit of this light curve yields a Lyman-
transit
depth of
%. The error bars are estimated using the
method
(see e.g., Hébrard et al. 2002), and using the same method
we can estimate the significance of the detection by calculating
the difference of
between the best fit and a fit
with no absorption at all (5th column of Table 3) or a fit
with an occultation by the planetary disk alone (6th column of Table 3).
Our result shows a transit depth that appears to be deeper
than the occultation by the planetary disk alone (
2.4%).
Using the statistical error bars, the excess absorption is at 3.5
level.
Of course, an unknown systematic effect mimicking a transit light curve with an excess
absorption cannot be excluded; nonetheless, the most likely explanation is the presence
of a huge cloud of atomic hydrogen surrounding HD 189733b.
The transit depths measured on individual light curves
of the transits #1 and #3 are different by about 2.5.
This difference
is clearly visible in the plot with data rebinned by four (Fig. 6).
4.2 Light curves in other lines
Table 4:
Results from light curves of emission lines other than H I Lyman-.
Using the same procedure as for Lyman-,
we measured the brightness of other stellar
emission lines and fit the light curves to measure the transit occultation depths
(Table 4). In these light curves, few measurements are obviously
outliers, in particular in the curve of the C I line.
These outliers have been removed by
flagging the points beyond 3
of the best fit. The number of points used for the
fit is given in the third column of Table 4.
We detect a transit signature in none of these lines.
Only upper limit on the transit depths can be derived.
For each line, the 3-
upper limit corresponds to
the transit depths that yield a
of 9 above the
of the best fit to the data.
For the two most important species (O I and C II), we obtain
a 3-
upper limit for the transit depth of about 11% and 5%,
respectively (Fig. 7). These two species
are abundant and light; therefore they should be, after hydrogen, the most abundant species
in the upper atmosphere. In contrast to the case of HD 209458b (Vidal-Madjar et al. 2004),
the non-detection of oxygen and carbon in the upper atmosphere of HD 189733b
precludes us from concluding anything about the nature of the escape mechanism
(see also Ben-Jaffel & Sona Hosseini 2010).
Note, however, that the lines from the ground level of
O I and C II are expected to be strongly
absorbed by the interstellar medium (see Fig. 2 of Vidal-Madjar et al. 2004),
so the observed stellar emission lines are mainly from
the excited levels O I*, O I**, and C II*.
Therefore, the upper limits quoted above should
be interpreted with caution, keeping in mind that
these levels are collisionally populated in gas with typical densities
above
106 cm-3.
4.3 Total flux redward of Lyman-
The planet transit cannot be seen in stellar emission lines
other than Lyman-
(Sect. 4.2). This is caused by the very low number of photons available in those lines. For instance, there are about
200 photons per exposure in the O I feature at 1305 Å; with a dozen of exposures
during the planetary transit, the accuracy of the transit depth is photon-noise
limited to about
2%.
This limitation can be overcome by the adding photons in a wide zone
of the spectra redward of the Lyman-
line, including
all these other emission lines and the stellar continuum together.
Using the range from 1280 Å to 1700 Å, we find about 3000 photons
per exposure (corresponding to about 0.5% photon-noise limit on the transit depth
measurement), to be compared
with the 1700 photons per exposure in the Lyman-
line.
We calculated the corresponding light curve (Figs. 8 and 9) and found a clear transit signature. In this light curve, we
also see a flare-like feature superimposed on the transit light
curve
.
This flare took place in the middle of the third visit, at the same epochs as
outliers already seen in light curves of individual lines, strengthening
the need for flagging those measurements.
For the spectra redward of Lyman-
,
if outliers beyond 3-
are flagged, we find a transit depth of
%, which is consitent with the transit of the planet
with a depth of 2.4% (Table 5).
This 4.6
-detection of the planet transit as expected
in such data gives confidence to the detection
of the transit seen at Lyman-
.
The calculated error bars on
the depths of both these detected transits are also consistent
with the theoretical limit from photon noise.
Finally, the detection of a flare in the middle of the third transit could explain
why the transit depth in Lyman-
is shallower in this last observation. If
the measurements obtained at the epoch of the flare are flagged (the epoch
of the 3 outliers at 3-
plus the two adjacent points),
we find a Lyman-
transit depth of
%. With this last
result, we would reach exactly the same conclusions.
Also, a careful inspection of individual measurements
does not show any hint of flare in Lyman-
(Fig. 4)
or in the O I line,
in contrast to carbon lines (C II plotted in Fig. 7 and C IV),
which show suspiciously large flux at the epoch of the flare.
This behavior is similar to what has been seen for solar flares, where large
variations are seen in C IV lines, while the Lyman-
line that originates
in a different part of the stellar atmosphere barely shows variations
(e.g., Brekket et al. 1996).
We conclude that the flare does not affect the main results of the present paper.
The detection of the transit of the planet in the spectra redward of Lyman-
strengthens the results at Lyman-
.
![]() |
Figure 7:
Plot of the flux in the C II line for the three HST transits. The data are photon-noise limited and the transit of the planet is not detected.
Only an upper limit on the transit depth can be obtained.
The solid line shows the transit light curve with the 3- |
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![]() |
Figure 8:
Plot of the flux redward of Lyman- |
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![]() |
Figure 9:
Plot of the flux redward of Lyman- |
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Table 5:
Results from the light curve redward of Lyman-.
5 Evaporation of HD 189733b
5.1 The stellar Lyman-
emission line profile
![]() |
Figure 10:
Plot of the theoretical spectrum of the Lyman- |
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As shown in Sect. 4.1, we detect a transit signature
in the light curve of the H I Lyman-
stellar emission line
with a depth of
5%, significantly deeper than the transit 2.4% depth due
to the planetary disk alone, as seen at optical wavelengths.
Moreover, the HD 189733b Lyman-
line is a broad emission line,
with a width of
150 km s-1.
From the experience with HD 209458b, we know that to interpret
this measurement we must consider the possibility
that the hydrogen cloud surrounding HD 189733b only absorbs
a fraction of this stellar line width.
Therefore the measured 5% absorption
depth in the total flux of the line is possibly caused by a larger absorption of
only a fraction of the line width (see discussion in Vidal-Madjar et al. 2008).
To interpret the measured absorption depth, it is therefore important
to have an estimate of the emission line width and shape.
The profile of the Lyman-
stellar emission line seen from Earth
is composed of the profile of the intrinsic stellar line combined with
the absorption by the interstellar atomic hydrogen and deuterium.
Interstellar hydrogen produced a narrow absorption at the line center.
Deuterium absorption is weaker and blueshifted by 80 km s-1.
The column density of atomic hydrogen toward HD 189733b is not known,
but a simple relation between the stars' distance and the H I column density
can be used. Using the results of Wood et al. (2005) and a distance of 19.3 pc
for HD 189733b, we infer an H I column of density,
,
of about
1018.3 cm-2.
Our conclusions are not sensitive to this assumption
because the column density for a star at
20 parsecs
is typically in the flat part of the curve of growth.
The core of the stellar line is fully absorbed by the cold interstellar medium.
The width of the stellar Lyman-
emission line is obtained using the
empirical relationship between the star absolute magnitude and the
chromospheric Lyman-
line FWHM (Landsman & Simon 1993).
This relation can be written as
,
where the width
is given in Ångstroms.
With an absolute
V magnitude of 6.1, we infer a line width of about 0.61 Å,
which is
km s-1, or for a Gaussian
= 64 km s-1.
We modeled the double peak chromospheric emission line with two Gaussians
of width
and separated by
.
Combined with the interstellar absorption, we obtained the profile of the
HD 189733 Lyman-
shown in Fig. 10.
5.2 HD 189733b is evaporating
We measure a 5% absorption depth over the broad Lyman-
line with a width of
150 km s-1, and this can
be interpreted by two extreme scenarios.
In the first scenario, the hydrogen cloud occults the full line width. In this case,
the 5% absorption corresponds to a cloud of about 1.65 Jupiter radii in size
with gas velocities reaching over 150 km s-1.
However, at 1.65 Jupiter radii the escape velocity from
HD 189733b is only 49 km s-1 (the escape velocity is 59 km s-1 at
one planetary radius). In this first scenario, the hydrogen
gas detected in the Lyman-
transit light curve exceeds the escape velocity, and
is therefore not gravitationally bound to the planet, so
the detected gas must be escaping.
In a second scenario, the velocity of the occulting gas
does not exceed the escape velocity, and so
the absorption only occurs in the core of the Lyman-
line.
Because only 1/6 of the observed Lyman-
flux comes from the core
of the line within the 49 km s-1 radial velocity limit, in this scenario
the absorption of the core must be at least 30% to produce a final absorption
of 5% in the full unresolved line.
A 30% absorption corresponds to a cloud of about 4 Jupiter radii in size, which
significantly exceeds the size of the Roche lobe of the planet (3.3 Jupiter radii).
In this second scenario, the gas detected in the Lyman-
transit light curve is beyond the Roche lobe, and
is therefore not gravitationally bound to the planet, so
the detected gas must be escaping.
An intermediate case between these two extreme scenarios can be
considered. Even if the Roche lobe was full of gas but
not beyond its borders,
and the gas velocity was up to the escape velocity but not above it,
the absorption depth would only be 3.3%. Therefore, the measured
5% absorption depth shows
that some gas must be either beyond the Roche lobe or at a velocity
above the escape velocity.
The reality is most likely in between the two extreme scenarios with both
a fraction of gas outside the Roche lobe and a fraction of gas at high velocity.
The present observations of a 5% absorption of the broad
Lyman-
emission line demonstrates that HD 189733b must be evaporating.
5.3 Numerical simulation
To interpret the H I light curve in more detail,
we modeled the atmospheric gas escaping HD 189733b with a numerical
simulation including the dynamics of the hydrogen atoms.
In this N-body simulation, hydrogen atoms are released from HD 189733b's upper
atmosphere
with a random initial velocity corresponding to a 10 000 K exobase.
This temperature corresponds to the temperature expected in the upper atmosphere
(e.g., Lecavelier des Etangs et al. 2004; Stone & Proga et al. 2009)
and has been actually measured for HD 209458b (Ballester et al. 2007).
In any case,
our results do not depend on this assumption because atoms are rapidly
accelerated by the radiation pressure to velocities several times higher
than their initial velocities.
In this model, the gravity of both the star and the planet are taken into account.
The radiation pressure from the stellar Lyman-
emission line is calculated
as a function of the radial velocity of the atoms.
The self-extinction within the cloud is also taken into account.
The hydrogen atoms are supposed to be ionized by the stellar extreme-UV (EUV). In the simulation, their lifetime is calculated as a function of the EUV flux, given as an input parameter to the model and expressed in solar units. The second input parameter is the atomic hydrogen escape rate, expressed in grams per second.
The dynamical model provides a steady state distribution of positions and velocities
of escaping hydrogen atoms in the cloud surrounding HD 189733b. From this information
we calculated the corresponding absorption over the stellar line and the corresponding
transit light curve of the total Lyman-
flux to be directly compared with the
observations.
5.4 Results
We calculated a grid of theoretical light curves as a function
of the two input parameters, namely the escape rate and
the EUV ionizing flux,
and compared them to the measured Lyman-
flux.
The EUV flux from HD 189733 has never been measured and is unknown. However,
for a K-type star, it can be estimated to be
in the range 1 to 100 times the solar EUV flux (e.g., Schmitt & Liefke 2004).
Using the theoretical light curves, we fitted the observational data
with the escape rate and EUV flux
as free parameters. For an escape rate below 107 g s-1, the occultation
by the HI cloud is negligible and the resulting Lyman-
light curve is similar to the planet occultation light curve with
a transit depth of
2.4% (Fig. 11).
For a large escape rate (
g s-1) and low EUV flux
(
3 times solar), the planet has a long trailing H I
cloud with a cometary shape, and the occultation is deeper and lasts
longer than the optical occultation by the planetary disk alone.
With these last conditions, the Lyman-
transit
depth exceeds 10% (Fig. 12).
Both the transit depth and duration constrains
the two parameters. Therefore,
the fit to the Lyman-
light curve can be used to
constrain both the escape rate and the ionizing flux
(Fig. 13).
We find that the data require an escape rate between
109 and 1011 g s-1 and an EUV flux
between 10 and 40 times the solar ionizing flux (1-
),
with larger escape rates corresponding to larger EUV flux
(Fig. 12).
The best fit is obtained for
g s-1 and
EUV flux
.
With these parameter values, the fit to the data with
the evaporating planet model yields a
of 91 for 80 degrees
of freedom (Fig. 11).
This fit is to be compared to the fit
with a model of a single optically-thick
disk for which we have a
of 97.9 for 81 degrees of freedom
(Table 3). Although the number of degrees of freedom is decreased
by one in the evaporating planet model (because there are two free parameters,
whereas only one parameter is needed to describe the size of the
optically-thick disk), this fit is significantly better
showing that the evaporating planet provides a
better scenario to explain the observational data.
![]() |
Figure 11:
Plot of the theoretical light curve of the total Lyman- |
Open with DEXTER |
![]() |
Figure 12:
Plot of the absorption depth on the theoretical light curve of the stellar H I Lyman- |
Open with DEXTER |
![]() |
Figure 13:
Plot of error bars for the estimated escape rate and EUV ionizing flux.
The best fit is obtained for
an escape rate of 1010 g s-1 and an ionizing EUV flux of 20 times solar.
To fit the data at 2 |
Open with DEXTER |
6 Discussion
The model used to interpret the H I transit light curve
assumes a given Lyman-
line width
of 0.61 Å (Sect 5.1).
This value is rather uncertain and might be underestimated
(Landsman & Simon 1993), and this is strengthened
by the particularly high chromospheric activity of
this star (Henry & Winn 2008; Boisse et al. 2009).
We tested this assumption by fitting the
data as in Sects. 5.3 and 5.4,
but using an FWMH of 1.0 Å for the simulated
HD 189733 Lyman-
stellar line. We found that, to fit the observed
light curve, a broader line requires a lower EUV ionizing flux,
because hydrogen atoms need to reach higher velocities
to occult the broader wings of the line before being ionized.
We found that an EUV ionizing flux between 2 and 10 times the solar value
and similar escape rates as in Sect. 5
provide a good fit to the data.
Taking the uncertainty on the Lyman-
line width into account,
we ended up with an EUV ionizing flux between 2 and 40 times the
solar value (1-
).
This test shows that the estimate of the escape rate is not sensitive to
the assumption on the width of the stellar emission line.
We constrained the escape rate of atomic hydrogen
to be about 1010 g s-1, which is similar to the
escape rate previously estimated in the case of HD 209458b.
The similarity between the two escape rates can be explained by comparing
the energy input by the stars and the physical properties of
the planets. In effect, theoretical models of the evaporation of
hot Jupiters agree to conclude that the escape rate can be
estimated by assuming that the EUV and X-ray energy input from the star is used by the
gas to escape the gravitation of the planet (Lecavelier des Etangs 2007).
The potential well of HD 189733b is about twice deeper than that of HD 209458b
(the planet mass is 1.7 larger, and the radius is 12% smaller).
However, this well
is largely compensated for by the orbital distance of HD 189733b which
is 1.5 times closer to its star than HD 209458b and the
stellar type of HD 189733 which as a K-type star is expected
to provide a higher EUV and X-ray input energy.
Within the uncertainties,
these orders of magnitude show that the similarity between
the observed evaporations of HD 189733b and HD 209458b
results from their similar physical properties.
In both cases, the observed escape rate is modest, and even if the escape of
ionized hydrogen is not detectable in Lyman-,
evaporation
is unlikely to change the nature of these two planets: 1010 g s-1
corresponds to the escape of about 0.2% of the planets' mass in 10 billion years.
However, the net effect of variations in EUV
flux on the observable is not obvious. In effect,
although an increased stellar EUV flux deposits more energy onto the
planetary upper atmosphere, and thereby increasing the heating and
consequently the atmospheric escape (e.g., Lecavelier des Etangs et al. 2004),
it is also more efficient at ionizing the escaping H I atoms,
hence reducing the size of the observable H I cloud
measured during the transit. This also contributes to
explaining why we find comparable absorption depths on
HD 189733b and HD 209458b, although their host stars
are of different stellar types.
Here it must be recalled that the transit depth is measured on
the Lyman-
line of atomic hydrogen and is interpreted in terms
of escape rate through a model in which the hydrogen ions are
produced by ionization by EUV stellar photons; therefore,
the quoted escape rates do not include escape of hydrogen ionized
by other mechanisms lower in the atmosphere.
We did not detect a transit signature of species other than hydrogen,
because of the photon noise limit on individual lines.
The transit signature can be seen by adding all photons redward of
the Lyman-
including all lines and the stellar continuum;
in this case the transit depth is consistent with the absorption
by the planetary disk alone.
With this limitation, it is not possible to conclude
anything about the escape mechanism, contrary to the case of HD 2908458 b
where detection of oxygen and carbon revealed
the hydrodynamical escape (``blow-off'') of the atmosphere
(Vidal-Madjar et al. 2004).
7 Conclusion
In summary, we have presented the 3.5
detection of an excess absorption
in the Lyman-
transit
light curve. This is interpreted in terms
of the evaporation in the upper atmosphere of HD 189733b. Any
detection at this level of confidence would call for an observational
confirmation, which will be possible with the repaired STIS
spectrograph. If confirmed, HD 189733b would be the second extrasolar
planet for which evaporation has been detected.
In the present observations, the Lyman-
line is not resolved,
removing any direct information on the radial velocity of the absorbing gas.
This limitation is due to the limited spectroscopic capabilities
of the ACS instrument in the far-ultraviolet, and the ACS was
used because of the STIS failure.
Fortunately, a significant improvement is expected after the refurbishment
of the Hubble Space Telescope performed last May 2009.
With the new Cosmic Origins Spectrograph (COS) and the repaired STIS,
new observations should allow us to address the issue of the escape mechanism
and to probe the dynamics of escaping atoms through an improved sensitivity
and sampling of the absorption along the Lyman-
line profile.
Finally, the results from each of the three observed transits
of HD 189733b are not exactly the same (Table 3).
Since the observations were obtained at different epochs (the last transit
was observed ten months later than the first two ones),
this raises the question of possible time variations in the transit depth.
From the present data, the detection of variations
is barely significant (2.5
),
and it may not be possible to draw definite conclusions
on this question.
Nonetheless, variations would not be surprising, at least
because of the expected variations in the EUV ionizing flux which,
for a given escape rate, significantly affects the observed transit depth (Fig. 12).
Interpretation of observations made at a single epoch is always tricky,
and any estimate or non-detection at a given time should never be considered
definitive.
We warmly thank F. Pont and F. Bouchy for useful comments and discussions, and A. Baillard and M. Dennefeld for their OHP observations of the HD 189733 field for preparing our HST observations.
Based on observations made with the NASA/ESA Hubble Space Telescope, obtained at the Space Telescope Science Institute, which is operated by the Association of Universities for Research in Astronomy, Inc., under NASA contract NAS 5-26555. These observations are associated with program GO10869.
D.E. acknowledges financial support from the French Agence Nationale pour la Recherche (ANR; project NT05-4_44463) and from the Centre National d'Études Spatiales (CNES). G.E.B. acknowledges financial support by this program through STScI grant HST-GO-10869.01-A to the University of Arizona.
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Footnotes
- ... Jupiters
- Usually defined as massive planets orbiting in less than 10 days.
- ... Jupiters
- Usually defined as planets orbiting in less than 3 days (e.g., Gaudi et al. 2005).
- ...
curve
- This flare-like feature looks similar to a flare seen at optical wavelength during the transit of the planet OGLE-TR-10b (Bentley et al. 2009). This topic will be discussed further in a separate paper.
All Tables
Table 1: Log of the observations. Time is given in UT.
Table 2: List of lines used to fit the 2D images.
Table 3:
Results from the Lyman-
light curve.
Table 4:
Results from light curves of emission lines other than H I Lyman-.
Table 5:
Results from the light curve redward of Lyman-.
All Figures
![]() |
Figure 1: 2D image of the HD 189733 spectrum obtained with ACS prism spectroscopy ( upper panel). The bottom panel shows the 2D-model of this image. In this image, stellar emission lines can be seen as bright spots: from left to right, the six brightest spots are the Lyman-alpha line, followed by the two O I and C II emission features, further to the right is the Si IV feature, and the two last spots are emission by C IV and C I. The stellar continuum emission is seen as a horizontal bright line along the spectrum. |
Open with DEXTER | |
In the text |
![]() |
Figure 2: Plot of the wavelength calibration. The squares show the position of each identified emission feature as a function of wavelength. The solid line shows the fit by a third-degree polynomial. |
Open with DEXTER | |
In the text |
![]() |
Figure 3: Plot of one-dimensional wavelength calibrated ACS spectrum of HD 189733. The brightest lines are identified. |
Open with DEXTER | |
In the text |
![]() |
Figure 4:
Lyman- |
Open with DEXTER | |
In the text |
![]() |
Figure 5:
Flux of the Lyman- |
Open with DEXTER | |
In the text |
![]() |
Figure 6: Same as previous plot in which the data have been rebinned by four. The possible difference of transit depth between different epochs are visible here. |
Open with DEXTER | |
In the text |
![]() |
Figure 7:
Plot of the flux in the C II line for the three HST transits. The data are photon-noise limited and the transit of the planet is not detected.
Only an upper limit on the transit depth can be obtained.
The solid line shows the transit light curve with the 3- |
Open with DEXTER | |
In the text |
![]() |
Figure 8:
Plot of the flux redward of Lyman- |
Open with DEXTER | |
In the text |
![]() |
Figure 9:
Plot of the flux redward of Lyman- |
Open with DEXTER | |
In the text |
![]() |
Figure 10:
Plot of the theoretical spectrum of the Lyman- |
Open with DEXTER | |
In the text |
![]() |
Figure 11:
Plot of the theoretical light curve of the total Lyman- |
Open with DEXTER | |
In the text |
![]() |
Figure 12:
Plot of the absorption depth on the theoretical light curve of the stellar H I Lyman- |
Open with DEXTER | |
In the text |
![]() |
Figure 13:
Plot of error bars for the estimated escape rate and EUV ionizing flux.
The best fit is obtained for
an escape rate of 1010 g s-1 and an ionizing EUV flux of 20 times solar.
To fit the data at 2 |
Open with DEXTER | |
In the text |
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