@InProceedings{NyassorWGPTBNBBFB:2019:CoGrWa,
author = "Nyassor, Prosper Kwamla and Wrasse, Cristiano Max and Gobbi,
Delano and Paulino, Igo and Takahashi, Hisao and Bageston,
Jos{\'e} Valentin and Naccarato, Kleber Pinheiro and Batista,
Paulo Prado and Barros, Diego and Figueiredo, Cosme Alexandre
Oliveira Barros and Buriti, Ricardo",
affiliation = "{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 (UFCG)} and {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 {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Universidade Federal de Campina Grande
(UFCG)}",
title = "Concentric Gravity Waves Observed by OH Airglow over Brazil",
year = "2019",
organization = "AGU Fall Meeting",
abstract = "We present first statistical results of concentric/circular
gravity waves (CGWs) observed in the OH airglow emission over the
Brazilian equatorial and low latitude regions. All-sky imagers
located at S{\~a}o Jo{\~a}o do Cariri [7.39°S, 36.53°W],
Petrolina [9.39°S, 40.50°W], Cachoeira Paulista [22.66°S, 45.00°W]
and S{\~a}o Martinho da Serra [29.48°S, 53.87°W] were used in the
acquisition of the images. Using 20 years of observational data
(between 1998 and 2018), 3525 nights of airglow observations were
taken. However, only 40 CGW(s) cases were found with small-scale
wave characteristics. The CGW(s) events showed horizontal
wavelengths between 20 and 40 km, horizontal phase speed between
40 and 107 m/s and periods ranging from 6 to 11 minutes. Most of
the CGW(s) structures were well defined with coherent wave
patterns expanding concentrically with 97.5% having semi-circle or
arc-like shapes. The occurrence of CGWs was found to coincide
mostly with the seasons of strong tropospheric convective activity
as well as low background winds, which corresponded to
non-solstice months. This suggested a low level of wave breaking
or critical level absorption/filtering, allowing the CGWs to
propagate up to the mesosphere and lower thermosphere (MLT)
region. The yearly latitudinal distribution of CGWs showed higher
occurrence in the subtropics (28°S), followed by the equatorial
latitudes (7°S) with the tropical latitudes (23°S) recording the
lowest occurrence.",
conference-location = "San Francisco, CA",
conference-year = "09-13 dec.",
language = "en",
targetfile = "nyassor_concentric.pdf",
urlaccessdate = "19 abr. 2024"
}