4.8 Article

Helium in the eroding atmosphere of an exoplanet

Journal

NATURE
Volume 557, Issue 7703, Pages 68-+

Publisher

NATURE PUBLISHING GROUP
DOI: 10.1038/s41586-018-0067-5

Keywords

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Funding

  1. STFC studentship
  2. European Research Council (ERC) under the European Union's Seventh Framework Programme (FP7)/ERC [336792]
  3. NASA programme of the STScI [HST-GO-14916]
  4. Tennessee State University
  5. State of Tennessee through its Centers of Excellence programme
  6. David and Lucille Packard Fellowship for Science and Engineering
  7. US National Science Foundation (NSF)
  8. John Templeton Foundation
  9. Swiss National Science Foundation (SNSF)
  10. SNSF
  11. ERC under the European Union's Horizon research and innovation programme (project FOUR ACES) [724427]
  12. NSF Graduate Research Fellowship [DGE-1746060]
  13. Earth in Other Solar Systems Team, NASA Nexus for Exoplanet System Science
  14. Leverhulme Trust Research Project Grant
  15. STFC [1636750] Funding Source: UKRI
  16. Division Of Astronomical Sciences
  17. Direct For Mathematical & Physical Scien [1616624] Funding Source: National Science Foundation

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Helium is the second-most abundant element in the Universe after hydrogen and is one of the main constituents of gas-giant planets in our Solar System. Early theoretical models predicted helium to be among the most readily detectable species in the atmospheres of exoplanets, especially in extended and escaping atmospheres(1). Searches for helium, however, have hitherto been unsuccessful(2). Here we report observations of helium on an exoplanet, at a confidence level of 4.5 standard deviations. We measured the near-infrared transmission spectrum of the warm gas giant(3) WASP-107b and identified the narrow absorption feature of excited metastable helium at 10,833 angstroms. The amplitude of the feature, in transit depth, is 0.049 +/- 0.011 per cent in a bandpass of 98 angstroms, which is more than five times greater than what could be caused by nominal stellar chromospheric activity. This large absorption signal suggests that WASP-107b has an extended atmosphere that is eroding at a total rate of 10(10) to 3 x 10(11) grams per second (0.1-4 per cent of its total mass per billion years), and may have a comet-like tail of gas shaped by radiation pressure.

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