4.8 Article

A continuum from clear to cloudy hot-Jupiter exoplanets without primordial water depletion

Journal

NATURE
Volume 529, Issue 7584, Pages 59-+

Publisher

NATURE PUBLISHING GROUP
DOI: 10.1038/nature16068

Keywords

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Funding

  1. European Research Council under the European Union's Seventh Framework Programme (FP7)/ERC [336792]
  2. STFC [ST/J0016/1]
  3. NASA from the STScI [HST-GO-12473]
  4. CNES
  5. French Agence Nationale de la Recherche (ANR) [ANR-12-BS05-0012]
  6. UK Science and Technology Facilities Council (STFC)
  7. NASA
  8. NSF
  9. Tennessee State University
  10. State of Tennessee through its Centers of Excellence programme
  11. STFC [ST/G002266/1, ST/J001627/1, ST/M003515/1, ST/N000919/1, ST/K00106X/1, ST/L000709/1] Funding Source: UKRI
  12. Science and Technology Facilities Council [ST/J001627/1, ST/L000709/1, ST/M003515/1] Funding Source: researchfish

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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(1-5). The low amplitude of water signatures could be explained by very low water abundances(6-8), which may be a sign that water was depleted in the protoplanetary disk at the planet's formation location9, 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(1-4), as found in some optical spectra(3,4,10,11). 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.

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