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

Jonathan B. Snively; Victor P. Pasko

doi:10.1029/2004GL022221

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

Jonathan B. Snively, Victor P. Pasko

Electrical Engineering

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18 Scopus citations

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 language	English (US)
Pages (from-to)	1-4
Number of pages	4
Journal	Geophysical Research Letters
Volume	32
Issue number	8
DOIs	https://doi.org/10.1029/2004GL022221
State	Published - Apr 28 2005

All Science Journal Classification (ASJC) codes

Geophysics
Earth and Planetary Sciences(all)

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10.1029/2004GL022221

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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.",

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AU - Pasko, Victor P.

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

Abstract

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