The Atmosphere of Pluto as Observed by New Horizons
arXiv:1604.05356 · doi:10.1126/science.aad8866
Abstract
Observations made during the New Horizons flyby provide a detailed snapshot of the current state of Pluto's atmosphere. While the lower atmosphere (at altitudes <200 km) is consistent with ground-based stellar occultations, the upper atmosphere is much colder and more compact than indicated by pre-encounter models. Molecular nitrogen (N) dominates the atmosphere (at altitudes <1800 km or so), while methane (CH), acetylene (CH), ethylene (CH), and ethane (CH) are abundant minor species, and likely feed the production of an extensive haze which encompasses Pluto. The cold upper atmosphere shuts off the anticipated enhanced-Jeans, hydrodynamic-like escape of Pluto's atmosphere to space. It is unclear whether the current state of Pluto's atmosphere is representative of its average state--over seasonal or geologic time scales.
arXiv commentin Science 351, aad8866 (2016)
References in corpus (15)
- The Pluto system: Initial results from its exploration by New Horizons
- Surface Compositions Across Pluto and Charon
- The Geology of Pluto and Charon Through the Eyes of New Horizons
- Ralph: A Visible/Infrared Imager for the New Horizons Pluto/Kuiper Belt Mission
- Long-Range Reconnaissance Imager on New Horizons
- Pluto's lower atmosphere structure and methane abundance from high-resolution spectroscopy and stellar occultations
- ALICE: The Ultraviolet Imaging Spectrograph aboard the New Horizons Pluto-Kuiper Belt Mission
- New Horizons: Anticipated Scientific Investigations at the Pluto System
- Near-Infrared Spectral Monitoring of Pluto's Ices: Spatial Distribution and Secular Evolution
- Plutos interaction with its space environment: Solar Wind, Energetic Particles & Dust
- Pluto's atmosphere from stellar occultations in 2012 and 2013
- In Situ Measurements of the Size and Density of Titan Aerosol Analogues
- Exploring the spatial, temporal, and vertical distribution of methane in Pluto's atmosphere
- Volatile transport on inhomogeneous surfaces: I. Analytic expressions, with application to Pluto's day
- Buoyancy waves in Pluto's high atmosphere: Implications for stellar occultations
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