SETI bioastro: FW: SwRI: Pluto Probe Finds "Dramatic Changes" in Jupiter's Moon Io

From: LARRY KLAES (ljk4_at_msn.com)
Date: Tue Oct 09 2007 - 10:26:29 PDT

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    >From: "AAS Press Officer Dr. Steve Maran" <Steve.Maran_at_aas.org>
    >To: "AAS Press Officer Dr. Steve Maran" <steve.maran_at_aas.org>
    >Subject: SwRI: Pluto Probe Finds "Dramatic Changes" in Jupiter's Moon Io
    >Date: Tue, 9 Oct 2007 11:13:43 -0400
    >

    THE FOLLOWING RELEASE WAS RECEIVED FROM THE SOUTHWEST RESEARCH INSTITUTE, IN
    SAN ANTONIO, TEXAS, AND IS FORWARDED FOR YOUR INFORMATION. (FORWARDING DOES
    NOT IMPLY ENDORSEMENT BY THE AMERICAN ASTRONOMICAL SOCIETY.) Steve Maran,
    American Astronomical Society steve.maran_at_aas.org 1-202-328-2010 x116

    Contact:
    Rob Leibold
    1-210-522-2258 rleibold_at_swri.org

    New Horizons’ Alice UV spectrograph observes Io’s atmosphere change in
    response to eclipse events

    SAN ANTONIO -- Oct. 9, 2007 -- Dramatic changes in the atmospheric density
    of Jupiter’s moon Io and its interaction with Jupiter’s magnetosphere
    during solar eclipse were observed through Io’s aurora on four occasions
    this past spring as the New Horizons spacecraft rounded Jupiter for a
    gravity assist on its way to Pluto.

    Scientists using New Horizons’ Southwest Research Institute
    (SwRI)-developed Alice ultraviolet spectrograph, which is designed to image
    ultraviolet emissions, noted auroral brightness and morphology variations as
    the spacecraft entered and then exited the eclipse zone revealing changes in
    the relative contribution of sublimation and volcanic sources to the
    atmosphere. The findings were supported by concurrent Hubble Space Telescope
    ultraviolet imaging and will be published in the Oct. 12 issue of Science.

    FUV (far-ultraviolet) aurora morphology also reveals the plumes effect on
    Io’s electrodynamic interaction with Jupiter’s magnetosphere.
    Comparisons to simulations of Io’s aurora indicate that volcanoes supply 1
    percent to 3 percent of Io’s dayside atmosphere.

    Aurora observations, particularly while Io is in solar eclipse by Jupiter,
    can provide information on both Io’s atmosphere and its interaction with
    Jupiter, the paper states.

    An aurora is a luminous phenomenon in the upper atmosphere of a planet
    caused by the emission of light from atoms excited by electrons accelerated
    along magnetic field lines. Most planetary aurorae occur in the polar
    regions, but Io’s aurora is brightest near its equator as well as in
    volcanic plumes distributed across the satellite.

    “Io is volcanically active, and that volcanism ultimately is the source
    material for Io’s sulfur-dioxide atmosphere, but the relative
    contributions of volcanic plumes and sublimation of frosts deposited near
    the plumes have remained a question for almost 30 years,” said Dr. Kurt
    Retherford, a senior research scientist in the Space Science and Engineering
    Division at the Institute.

    The interaction between Io’s atmosphere and the Io plasma torus produces
    displays of auroral emissions on Io, supplies plasma to Jupiter’s
    magnetosphere and physically links Io to Jupiter, according to the paper.

    “When Io goes into solar eclipse, and during the night, its surface
    temperature drops significantly, causing diminished sublimation of surface
    material into the atmosphere. The atmosphere at that point collapses down so
    that all that is left supplying the atmosphere are the volcanoes,”
    Retherford said.

    A dramatic difference between Io’s dayside and nightside atmospheric
    density best explains the aurorae observations, he added.

    Alice provides spectral images in the extreme- and far-ultraviolet (EUV and
    FUV) passbands. S. Alan Stern, NASA’s associate administrator for the
    Science Mission Directorate and former executive director of the Space
    Science and Engineering Division at SwRI, is the principal investigator of
    New Horizons, Alice and Ralph, a visible and infrared camera onboard the
    spacecraft. Prof. Joachim Saur at the University of Cologne, Germany,
    conducted the simulations.

    New Horizons is the first mission in NASA’s New Frontiers program. The
    Johns Hopkins University Applied Physics Laboratory manages the mission and
    operates the spacecraft for the NASA Science Mission Directorate. SwRI leads
    the SWAP instrument and hosts the Tombaugh Science Operations Center.

    The paper is titled, “Io’s Atmospheric Response to Eclipse: UV Aurorae
    Observations,” by K.D. Retherford, J.R. Spencer, S.A. Stern, J. Saur, D.F.
    Strobel, A.J. Steffl, G.R. Gladstone, H.A. Weaver, A.F. Cheng, J.Wm. Parker,
    D.C. Slater, M.H. Versteeg, M.W. Davis, F. Bagenal, H.B. Throop, R.M.C.
    Lopes, D.C. Reuter, A. Lunsford, S.J. Conard, L.A. Young and J.M. Moore.

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