Antiphase OH and OI airglow emissions induced by a short-period ducted gravity wave

Jonathan B. Snively, Victor P. Pasko

    Research output: Contribution to journalArticle

    18 Citations (Scopus)

    Abstract

    Numerical simulation of a ducted gravity wave event suggests that OH (8,3) and O(1S) 557.7 nm airglow emissions layers may exhibit opposite-phase intensities when perturbed by a short-period wave undergoing vertical reflection. This effect arises due to the time and temperature dependance of the OH excitation reaction, coupled with the linear polarization properties of vertically-standing waves.

    Original languageEnglish (US)
    Pages (from-to)1-4
    Number of pages4
    JournalGeophysical Research Letters
    Volume32
    Issue number8
    DOIs
    StatePublished - Apr 28 2005

    Fingerprint

    airglow
    standing wave
    gravity waves
    linear polarization
    standing waves
    gravity wave
    polarization
    excitation
    simulation
    temperature
    effect

    All Science Journal Classification (ASJC) codes

    • Earth and Planetary Sciences (miscellaneous)

    Cite this

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    Antiphase OH and OI airglow emissions induced by a short-period ducted gravity wave. / Snively, Jonathan B.; Pasko, Victor P.

    In: Geophysical Research Letters, Vol. 32, No. 8, 28.04.2005, p. 1-4.

    Research output: Contribution to journalArticle

    TY - JOUR

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    AU - Snively, Jonathan B.

    AU - Pasko, Victor P.

    PY - 2005/4/28

    Y1 - 2005/4/28

    N2 - Numerical simulation of a ducted gravity wave event suggests that OH (8,3) and O(1S) 557.7 nm airglow emissions layers may exhibit opposite-phase intensities when perturbed by a short-period wave undergoing vertical reflection. This effect arises due to the time and temperature dependance of the OH excitation reaction, coupled with the linear polarization properties of vertically-standing waves.

    AB - Numerical simulation of a ducted gravity wave event suggests that OH (8,3) and O(1S) 557.7 nm airglow emissions layers may exhibit opposite-phase intensities when perturbed by a short-period wave undergoing vertical reflection. This effect arises due to the time and temperature dependance of the OH excitation reaction, coupled with the linear polarization properties of vertically-standing waves.

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