Abstract
Thousands of transiting exoplanets have been discovered, but spectral
analysis of their atmospheres has so far been dominated by a small
number of exoplanets and data spanning relatively narrow wavelength
ranges (such as 1.1-1.7 micrometres). Recent studies show that
some hot-Jupiter exoplanets have much weaker water absorption features
in their near-infrared spectra than predicted. The low amplitude of
water signatures could be explained by very low water abundances, which
may be a sign that water was depleted in the protoplanetary disk at the
planet’s formation location, but it is unclear whether this level
of depletion can actually occur. Alternatively, these weak signals could
be the result of obscuration by clouds or hazes, as found in some
optical spectra. Here we report results from a comparative study of ten
hot Jupiters covering the wavelength range 0.3-5 micrometres,
which allows us to resolve both the optical scattering and infrared
molecular absorption spectroscopically. Our results reveal a diverse
group of hot Jupiters that exhibit a continuum from clear to cloudy
atmospheres. We find that the difference between the planetary radius
measured at optical and infrared wavelengths is an effective metric for
distinguishing different atmosphere types. The difference correlates
with the spectral strength of water, so that strong water absorption
lines are seen in clear-atmosphere planets and the weakest features are
associated with clouds and hazes. This result strongly suggests that
primordial water depletion during formation is unlikely and that clouds
and hazes are the cause of weaker spectral signatures.
Original language | English |
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Pages (from-to) | 59-62 |
Number of pages | 4 |
Journal | Nature |
Volume | 529 |
Issue number | 7584 |
Early online date | 14 Dec 2015 |
DOIs | |
Publication status | Published - 07 Jan 2016 |
Externally published | Yes |