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A bimodal distribution of haze in Pluto’s atmosphere

Siteng Fan (), Peter Gao, Xi Zhang, Danica J. Adams, Nicholas W. Kutsop, Carver J. Bierson, Chao Liu, Jiani Yang, Leslie A. Young, Andrew F. Cheng and Yuk L. Yung
Additional contact information
Siteng Fan: California Institute of Technology
Peter Gao: Carnegie Institution for Science
Xi Zhang: University of California Santa Cruz
Danica J. Adams: California Institute of Technology
Nicholas W. Kutsop: Cornell University
Carver J. Bierson: University of California Santa Cruz
Chao Liu: California Institute of Technology
Jiani Yang: California Institute of Technology
Leslie A. Young: Southwest Research Institute
Andrew F. Cheng: Johns Hopkins University Applied Physics Laboratory
Yuk L. Yung: California Institute of Technology

Nature Communications, 2022, vol. 13, issue 1, 1-11

Abstract: Abstract Pluto, Titan, and Triton make up a unique class of solar system bodies, with icy surfaces and chemically reducing atmospheres rich in organic photochemistry and haze formation. Hazes play important roles in these atmospheres, with physical and chemical processes highly dependent on particle sizes, but the haze size distribution in reducing atmospheres is currently poorly understood. Here we report observational evidence that Pluto’s haze particles are bimodally distributed, which successfully reproduces the full phase scattering observations from New Horizons. Combined with previous simulations of Titan’s haze, this result suggests that haze particles in reducing atmospheres undergo rapid shape change near pressure levels ~0.5 Pa and favors a photochemical rather than a dynamical origin for the formation of Titan’s detached haze. It also demonstrates that both oxidizing and reducing atmospheres can produce multi-modal hazes, and encourages reanalysis of observations of hazes on Titan and Triton.

Date: 2022
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DOI: 10.1038/s41467-021-27811-6

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