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    Spectroscopic anatomy of a meteor trail cross section with the European Southern Observatory Very Large Telescope

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    Author
    Jenniskens, P.
    Jehin, E.
    Cabanac, R. A.
    Laux, C. O.
    Boyd, I. D.
    Issue Date
    2004-01-01
    Keywords
    Aerothermochemistry
    carbonates
    ESO/VLT
    Meteor trail width
    Prebiotic chemistry
    
    Metadata
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    Citation
    Jenniskens, P., Jehin, E., Cabanac, R. A., Laux, C. O., & Boyd, I. D. (2004). Spectroscopic anatomy of a meteor trail cross section with the European Southern Observatory Very Large Telescope. Meteoritics & Planetary Science, 39(4), 609-616.
    Publisher
    The Meteoritical Society
    Journal
    Meteoritics & Planetary Science
    URI
    http://hdl.handle.net/10150/656680
    DOI
    10.1111/j.1945-5100.2004.tb00923.x
    Additional Links
    https://meteoritical.org/
    Abstract
    A meteor spectrum was recorded serendipitously at the European Southern Obrervatory (ESO) Very Large Telescope (VLT) during a long exposure in long-slit spectroscopic mode with FORS1. The -8 magnitude fireball crossed the narrow 1Î x 7î slit during the observation of a high z supernova in normal service mode operation on May 12, 2002. The spectrum covered the range of 6371050 nm, where the meteors air plasma emissions from N2, N, and O dominate. Carbon atom emission was not detected in the relatively unexplored wavelength range above 900 nm, but the observed upper limit was only 3 sigma less than expected from the dissociation of atmospheric CO2. The meteor trail was resolved along the slit, and the emission had a Gaussian distribution with a dimension of FWHM = 7.0 (+/- 0.4) * sin(alpha) * H (km)/90 m, where alpha is the unknown angle between the orientation of the meteor path and slit and H the assumed altitude of the meteor in km. To our knowledge, this is the first observation of a spatially resolved spectrum across a meteor trail. Unlike model predictions, the plasma excitation temperature varied only from about 4,300 to 4,365 K across the trail, based on the ratio of atomic and molecular nitrogen emissions. Unfortunately, we conclude that this was because the meteor at 100 km altitude was out of focus.
    Type
    Article
    text
    Language
    en
    ISSN
    1945-5100
    ae974a485f413a2113503eed53cd6c53
    10.1111/j.1945-5100.2004.tb00923.x
    Scopus Count
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    Meteoritics & Planetary Science, Volume 39, Number 4 (2004)

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