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Title: A TRANSMISSION SPECTRUM OF TITAN'S NORTH POLAR ATMOSPHERE FROM A SPECULAR REFLECTION OF THE SUN

Journal Article · · Astrophysical Journal
 [1];  [2]; ;  [3];  [4]; ;  [5];  [6];  [7];  [8];  [9]
  1. Department of Physics, University of Idaho, Moscow, ID 83844-0903 (United States)
  2. United States Geological Survey, Denver, CO 80225 (United States)
  3. Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Dr., Pasadena, CA 91109 (United States)
  4. Department of Astronomy, University of California Berkeley, Berkeley, CA 94720-3411 (United States)
  5. Laboratoire AIM, Université Paris Diderot, Paris 7/CNRS/CEA-Saclay, DSM-IRFU/SAp, F-91191 Gif sur Yvette (France)
  6. Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139-4307 (United States)
  7. Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721 (United States)
  8. Space Science and Engineering Center, University of Wisconsin-Madison, Madison, WI, 53706 (United States)
  9. Laboratoire de Planétologie et Géodynamique, Université de Nantes, F-44322 Nantes (France)

Cassini/VIMS T85 observations of a solar specular reflection off of Kivu Lacus (87.°4N 241.°1E) provide an empirical transmission spectrum of Titan's atmosphere. Because this observation was acquired from short range (33,000 km), its intensity makes it visible within the 2.0, 2.7, and 2.8 μm atmospheric windows in addition to the 5 μm window where all previous specular reflections have been seen. The resulting measurement of the total one-way normal atmospheric optical depth (corresponding to haze scattering plus haze and gas absorption) provides strong empirical constraints on radiative transfer models. Using those models, we find that the total haze column abundance in our observation is 20% higher than the Huygens equatorial value. Ours is the first measurement in the 2-5 μm wavelength range that probes all the way to the surface in Titan's arctic, where the vast majority of surface liquids are located. The specular technique complements other probes of atmospheric properties such as solar occultations and the direct measurements from Huygens. In breaking the degeneracy between surface and atmospheric absorptions, our measured optical depths will help to drive future calculations of deconvolved surface albedo spectra.

OSTI ID:
22270547
Journal Information:
Astrophysical Journal, Vol. 777, Issue 2; Other Information: Country of input: International Atomic Energy Agency (IAEA); ISSN 0004-637X
Country of Publication:
United States
Language:
English

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