A global cloud map of the nearest known brown dwarf

I. J. M. Crossfield*, B. Biller, J. E. Schlieder, N. R. Deacon, M. Bonnefoy, D. Homeier, F. Allard, E. Buenzli, Th. Henning, W. Brandner, B. Goldman, T. Kopytova

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

Abstract / Description of output

Brown dwarfs—substellar bodies more massive than planets but not massive enough to initiate the sustained hydrogen fusion that powers self-luminous stars1,2—are born hot and slowly cool as they age. As they cool below about 2,300 kelvin, liquid or crystalline particles composed of calcium aluminates, silicates and iron condense into atmospheric ‘dust’3,4, which disappears at still cooler temperatures (around 1,300 kelvin) 5,6. Models to explain this dust dispersal include both an abrupt sinking of the entire cloud deck into the deep, unobservable atmosphere5,7 and breakup of the cloud into scattered patches 6,8 (as seen on Jupiter and Saturn9). However, hitherto observations of brown dwarfs have been limited to globally integrated measurements10, which can reveal surface inhomogeneities but cannot unambiguously resolve surface features11. Here we report a two-dimensional map of a brown dwarf’s surface that allows identification of large-scale bright and dark features, indicative of patchy clouds. Monitoring suggests that the characteristic timescale for the evolution of global weather patterns is approximately one day.

Original languageEnglish
Pages (from-to)654–656
Number of pages3
Issue number7485
Early online date29 Jan 2014
Publication statusPublished - 30 Jan 2014

Keywords / Materials (for Non-textual outputs)

  • WISE J104915.57-531906.1AB
  • HD 189733B
  • 2 PC
  • MU-M


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