Brown dwarfs -interstellar bodies more massive than planets but not massive enough to initiate the sustained hydrogen fusion that powers self-luminous stars 1,2 -are born hot and slowly cool as they age. As they cool below ~2300 K, liquid or crystalline particles composed of calcium aluminates, silicates, and/or iron condense into atmospheric "dust" 3,4 which disappears at still cooler temperatures (~1300 K) 5,6 . Models to explain this dust dispersal include both an abrupt sinking of the entire cloud deck into the deep, unobservable atmosphere 5,7 or breakup of the cloud into scattered patches 6,8 (as seen on Jupiter and Saturn 9 ), but to date observations of brown dwarfs have been limited to globally integrated measurements 10 ; such measurements can reveal surface inhomogeneities but cannot unambiguously resolve surface features 11 . Here we report a twodimensional map of a brown dwarf's surface that allows identification of large-scale bright and dark features, indicative of patchy clouds. Geographic localization of such features, and the ability to create timelapsed extrasolar weather movies in the near future, provide important new constraints on the formation, evolution, and dispersal of clouds in brown dwarf and extrasolar planet atmospheres.The recent discovery of the Luhman 16AB system (also called WISE J104915.57-531906.1AB; Ref. 12) revealed two brown dwarfs only 2 parsecs away, making these the closest objects to the Solar system after the alpha Centauri system and Barnard's star. Both of these newly-discovered brown dwarfs are near the dust clearing temperature 13,14 , and one (Luhman 16B) exhibits strong temporal variability of its thermal radiation consistent with a rotation period of 4.9 hr
15. Luhman 16AB's proximity to Earth makes these the first substellar objects bright enough to be studied at high precision and high spectral resolution on short timescales, so we observed both of these brown dwarfs for five hours (one rotation period of Luhman 16B) using the CRIRES spectrograph 16 at ESO's Very Large Telescope to search for spectroscopic variability.
of 17Absorption features from CO and H2O dominate the brown dwarfs' spectra, as shown in Fig. 1. The two objects have similar spectra but the absorption lines are broader for the B component: it exhibits a projected equatorial rotational velocity of 26.1 +/-0.2 km/s, vs. 17.6 +/-0.1 km/s for Luhman 16A. Taking Luhman 16B's rotation period 15 and considering that evolutionary models predict these objects to be 1.0+/-0.2 times the radius of Jupiter 17 , Luhman 16B's rotation axis must be inclined ≲30 deg from the plane of the sky; i.e., we are viewing this brown dwarf nearly equator-on. If the two brown dwarfs' axes are closely aligned (like those of the planets in our Solar system) then Luhman 16A rotates more slowly than Luhman 16B and the objects either formed with different initial angular momentum or experienced different accretion or spin-braking histories. Alternatively, if the two brown dwarfs have comparable rotation periods (as tentativ...