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Simultaneous observation of ionospheric plasma bubbles and mesospheric gravity waves during the SpreadFEx Campaign

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TLDR
In this article, two airglow CCD imagers, located at Cariri (7.4° S, 36.5° W, geomag. 11° S) and near Brasilia (14.8°S, 47.6°W, geOMag. 10°S) were operated simultaneously and measured the equatorial ionospheric bubbles and their time evolution by monitoring the airglove OI 6300 intensity depletions.
Abstract
. During the Spread F Experiment campaign, under NASA Living with a Star (LWS) program, carried out in the South American Magnetic Equator region from 22 September to 8 November 2005, two airglow CCD imagers, located at Cariri (7.4° S, 36.5° W, geomag. 11° S) and near Brasilia (14.8° S, 47.6° W, geomag. 10° S) were operated simultaneously and measured the equatorial ionospheric bubbles and their time evolution by monitoring the airglow OI 6300 intensity depletions. Simultaneous observation of the mesospheric OH wave structures made it possible to investigate the relationship between the bubble formation in the ionosphere and the gravity wave activity at around 90 km. On the evening of 30 September 2005, comb-like OI 6300 depletions with a distance of ~130 km between the adjacent ones were observed. During the same period, a mesospheric gravity wave with a horizontal wavelength of ~130 km was observed. From the 17 nights of observation during the campaign period, there was a good correlation between the OI 6300 depletion distances and the gravity wave horizontal wavelengths in the mesosphere with a statistically significant level, suggesting a direct contribution of the mesospheric gravity wave to plasma bubble seeding in the equatorial ionosphere.

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Journal ArticleDOI

Quiescent prominence dynamics observed with the hinode solar optical telescope. i. turbulent upflow plumes

TL;DR: In this paper, a detailed kinematic measurement of the small-scale turbulent upflows seen in several prominences in the SOT database is presented, and the authors conclude that buoyant plumes are a source of quiescent prominence mass as well as a mechanism by which prominence plasma is advected upward.
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Internal wave coupling processes in Earth's atmosphere

TL;DR: A review of vertical coupling in the atmosphere and ionosphere system induced by internal waves of lower atmospheric origin is presented in this article, focusing on gravity waves, solar tides, planetary Rossby and Kelvin waves.
Journal ArticleDOI

Gravity wave initiation of equatorial spread F/plasma bubble irregularities based on observational data from the SpreadFEx campaign

TL;DR: In this paper, the role of gravity waves in the instability initiation leading to equatorial spread F development was investigated using ground-based experiments conducted during the 2005 SpreadFEx campaign in Brazil.
Journal ArticleDOI

Numerical Simulations of the Magnetic Rayleigh-Taylor Instability in the Kippenhahn-Schlüter Prominence Model. I. Formation of Upflows

TL;DR: In this article, the authors investigate the nonlinear stability of the Kippenhahn-Schluter prominence model for the interchange mode of the magnetic Rayleigh-Taylor instability.
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Gravity wave and tidal influences on equatorial spread F based on observations during the Spread F Experiment (SpreadFEx)

TL;DR: In this paper, the authors used the results of the SpreadFEx campaign to estimate gravity wave characteristics at the bottomside F layer, and to assess their possible con- tributions to optimal seeding conditions for equatorial spread F and plasma instability growth rates.
References
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An introduction to dynamic meteorology

TL;DR: The instructor's manual to a work which introduces the fundamental principles of meteorology, explaining storm dynamics and the dynamics of climate and its global implications is described in this article, where the authors present a detailed discussion of the relationship between meteorology and climate.
Journal ArticleDOI

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