@Article{KheraniAbPaFrSoMe:2009:ImGrWa,
author = "Kherani, E. Alam and Abdu, Mangalathayil Ali and Paula, Eurico
Rodrigues de and Fritts, D. C. and Sobral, Jos{\'e} Humberto
Andrade and Meneses Junior, F. C.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)}",
title = "The impact of gravity waves rising from convection in the lower
atmosphere on the generation and nonlinear evolution of equatorial
bubble",
journal = "Annales Geophysicae",
year = "2009",
volume = "27",
number = "4",
pages = "1657--1668",
keywords = "Ionosphere, Ionospheric irregularities, Plasma waves and
instabilities.",
abstract = "The nonlinear evolution of equatorial F-region plasma bubbles
under varying ambient ionospheric conditions and gravity wave
seeding perturbations in the bottom-side F-layer is studied. To do
so, the gravity wave propagation from the convective source region
in the lower atmosphere to the thermosphere is simulated using a
model of gravity wave propagation in a compressible atmosphere.
The wind perturbation associated with this gravity wave is taken
as a seeding perturbation in the bottomside F-region to excite
collisional-interchange instability. A nonlinear model of
collisional-interchange instability (CII) is implemented to study
the influences of gravity wave seeding on plasma bubble formation
and development. Based on observations during the SpreadFEx
campaign, two events are selected for detailed studies. Results of
these simulations suggest that gravity waves can play a key role
in plasma bubble seeding, but that they are also neither necessary
nor certain to do so. Large gravity wave perturbations can result
in deep plasma bubbles when ionospheric conditions are not
conducive by themselves; conversely weaker gravity wave
perturbations can trigger significant bubble events when
ionospheric conditions are more favorable. But weak gravity wave
perturbations in less favorable environments cannot, by
themselves, lead to strong plasma bubble responses.",
issn = "0992-7689",
language = "en",
urlaccessdate = "11 maio 2024"
}