@InProceedings{FechineTaWrGoMeMlRu:2006:MeInLa,
author = "Fechine, Joaquim and Takahashi, Hisao and Wrasse, Cristiano Max
and Gobbi, Delano and Medeiros, A. F. and Mlynczak, M. G. and
Russel, J. M.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Universidade Federal de Campina Grande} and
Atmospheric Sciences Division, NASA and Atmospheric Sciences
Division, NASA",
title = "Mesospheric inversion layers and gravity wave activity over
Brazilian equatorial region",
booktitle = "Proceedings...",
year = "2006",
organization = "Committe on Space Research, 36. (COSPAR).",
abstract = "During the last five years mesospheric gravity wave activities
have been observed using an all-sky imager at S{\~a}o Jo{\~a}o
do Cariri (7.4S, 36.5W), Brazil. Among these waves, particularly
interesting phenomenon is mesospheric front whose origin and
physics are not well known. The mesospheric front is a well
defined leading edge of the airglow emission layer, that is,
spatially extended and pronounced in. It is suggested that the
development of these fronts is strongly associated with the MLT
thermal structure. In the present paper we will use kinetic
temperature profile data obtained by TIMED/SABER satellite to
discuss the atmospheric background conditions where the
mesospheric fronts propagate.",
conference-location = "Beijing, China",
conference-year = "2006-07-16",
label = "self-archiving-INPE-MCTIC-GOV-BR",
language = "en",
targetfile = "fechine_mesospheric.pdf",
urlaccessdate = "03 maio 2024"
}