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AGU: Geophysical Research Letters

 

Keywords

  • Cassini
  • Titan
  • ultraviolet

Index Terms

  • Planetary Sciences: Solar System Objects: Titan
  • Planetary Sciences: Comets and Small Bodies: Aurorae, airglow, and X-ray emission
  • Atmospheric Composition and Structure: Airglow and aurora

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 34, L24204, 5 PP., 2007
doi:10.1029/2007GL031555

Titan airglow spectra from Cassini Ultraviolet Imaging Spectrograph (UVIS): EUV analysis

Joseph M. Ajello

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

Michael H. Stevens

Space Science Division, Naval Research Laboratory, Washington, D. C., USA

Ian Stewart

Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, Colorado, USA

Kristopher Larsen

Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, Colorado, USA

Larry Esposito

Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, Colorado, USA

Josh Colwell

Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, Colorado, USA

Science Department, Central Arizona College, Coolidge, Arizona, USA

William McClintock

Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, Colorado, USA

Greg Holsclaw

Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, Colorado, USA

Jacques Gustin

Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, Colorado, USA

Wayne Pryor

Science Department, Central Arizona College, Coolidge, Arizona, USA

We present the first UV airglow observations of Titan's atmosphere by the Ultraviolet Imaging Spectrograph (UVIS) on Cassini. Using one spectral channel in the EUV from 561–1182 Å and one in the FUV from 1115–1913 Å, UVIS observed the disk on 13 December, 2004 at low solar activity. The EUV spectrum consists of three band systems of N2 (b 1u, b′ 1u +, c41u + → X 1g +), while the FUV spectrum consists of one (a 1g → X 1g +). Both the EUV and FUV spectra contain many N I and N II multiplets that are produced primarily by photodissociative ionization. Spectral intensities of the N2 c41u +(v′ = 0) → X 1g +(v″ = 0–2) progression from 950–1010 Å are resolved for the first time. The UVIS observations reveal that the c41u +(0) → X 1g + (0) vibrational band near 958 Å is weak and undetectable, and that N I multiplets near 953.2 and 964.5 Å are present instead. Magnetospheric particle excitation may be weak or sporadic, since the nightside EUV spectrum on this orbit shows no observable nitrogen emission features and only H Ly-β.

Received 6 August 2007; accepted 15 October 2007; published 25 December 2007.

Citation: Ajello, J. M., M. H. Stevens, I. Stewart, K. Larsen, L. Esposito, J. Colwell, W. McClintock, G. Holsclaw, J. Gustin, and W. Pryor (2007), Titan airglow spectra from Cassini Ultraviolet Imaging Spectrograph (UVIS): EUV analysis, Geophys. Res. Lett., 34, L24204, doi:10.1029/2007GL031555.

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