@Article{NyassorWPSBNGFATS:2022:SoCoGr,
author = "Nyassor, Prosper Kwamla and Wrasse, Cristiano Max and Paulino, Igo
and S{\~a}o Sabbas, Eliah Fernanda de Maria de and Bageston,
Jos{\'e} Valentin and Naccarato, Kleber Pinheiro and Gobbi,
Delano and Figueiredo, Cosme Alexandre Oliveira Barros and
Ayorinde, Toyese Tunde and Takahashi, Hisao and Silva, Diego
Barros",
affiliation = "{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 {} and {Instituto Nacional de
Pesquisas Espaciais (INPE)}",
title = "Sources of Concentric Gravity Waves Generated by a Moving
Mesoscale Convective System in Southern Brazi",
journal = "Atmospheric Chemistry and Physics Discussions",
year = "2022",
volume = "2022",
keywords = "The studies on the sources of three concentric gravity waves
(CGWs) excited by a moving Mesoscale Convective System (MCS) on
the night of October 1 - 2, 2019 are investigated. These CGWs were
observed using an OH all-sky imager whereas the MCS were observed
by the Geostationary Operational Environmental Satellite (GOES).
Using 2D spectral analysis, we observed that the CGWs have
horizontal wavelength \λ,, , H \∼,, , 30 - 55 km, phase
speed cH \∼,, , 70 - 90 m/s, and period \τ,, ,
\∼,, , 7 - 12 min. By backward ray tracing we found that two
of the waves were excited from convective cores within the MCS. We
also found that the epicenters of the CGWs were close to the
tropopause positions of the ray traced paths as well as the nearby
convective cores. Regarding the source, we verified that on this
night the cold-point tropopause (CPT) was \∼,, ,
-80\◦,, , C, which was \∼,, , 10\◦,, , C cooler
than CPT on the days preceding and after the MCS, and also colder
than usually observed. Since the tropopause height and temperature
are fundamental parameters underlying the analysis of the
overshooting extent, we developed our own methodology to establish
a reference tropopause that would enable a quantitative estimate
of this parameter. Since the MCS, (CGWs source) was moving, the
overshooting convective cores were tracked in space and time.
Finally, we found that two out, of the three CGWs were excited by
the MCS whereas the source of the remaining one was found not to
be directly associated, with the MCS.",
doi = "10.5194/acp-2022-267",
url = "http://dx.doi.org/10.5194/acp-2022-267",
issn = "1680-7367",
language = "en",
targetfile = "acp-2022-267.pdf",
urlaccessdate = "27 abr. 2024"
}