@PhDThesis{Moura:2018:MeEsCa,
author = "Moura, Regiane",
title = "Mecanismos de estabilidade da camada limite atmosf{\'e}rica
marinha na regi{\~a}o da conflu{\^e}ncia Brasil-Malvinas",
school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
year = "2018",
address = "S{\~a}o Jos{\'e} dos Campos",
month = "2017-11-27",
keywords = "conflu{\^e}ncia Brasil-Malvinas, camada limite atmosf{\'e}rica
marinha, WRF, COAWST, equa{\c{c}}{\~a}o de tend{\^e}ncia de
momentum, Brasil Malvinas confluence, marine atmospheric boundary
layer, WRF, COAWST, momentum budget tendency.",
abstract = "Os efeitos da frente t{\'e}rmica oce{\^a}nica na Camada Limite
Atmosf{\'e}rica Marinha, na regi{\~a}o da Conflu{\^e}ncia
BrasilMalvinas, foram estudados em dois casos de intensidade do
gradiente de TSM distintos, um mais intenso e outro menos intenso,
e sob duas condi{\c{c}}{\~o}es atmosf{\'e}ricas diferentes.
Utilizando modelos num{\'e}ricos de alta resolu{\c{c}}{\~a}o,
foram analisados os processos din{\^a}micos e termodin{\^a}micos
em transectos perpendiculares e paralelos ao gradiente de TSM. O
objetivo principal deste estudo foi analisar em quais
condi{\c{c}}{\~o}es os mecanismos de mistura vertical e ajuste
de press{\~a}o ocorrem na CLAM. Atrav{\'e}s dos termos da
equa{\c{c}}{\~a}o de momentum e fluxos de calor, p{\^o}dese
observar que os mecanismos de ajuste de press{\~a}o e mistura
vertical coexistem sob as duas condi{\c{c}}{\~o}es
sin{\'o}ticas analisadas e operam de diferentes maneiras de um
lado e de outro da frente de TSM. Sob atua{\c{c}}{\~a}o de um
sistema de alta press{\~a}o atmosf{\'e}rica em
superf{\'{\i}}cie, a CLAM {\'e} modulada localmente pela TSM e
responde {\`a} for{\c{c}}ante t{\'e}rmica, no qual os termos de
ordem menor da equa{\c{c}}{\~a}o de tend{\^e}ncia podem ser
negligenciados, j{\'a} que tratase de uma situa{\c{c}}{\~a}o de
equil{\'{\i}}brio quasegeostr{\'o}fico. Por outro lado, sob a
atua{\c{c}}{\~a}o de um sistema de baixa press{\~a}o
atmosf{\'e}rica superficial, a CLAM {\'e} influenciada por
mecanismos din{\^a}micos, nos quais os termos de
fric{\c{c}}{\~a}o e advec{\c{c}}{\~a}o est{\~a}o na mesma
ordem da for{\c{c}}a gradiente de press{\~a}o. ABSTRACT: The
effects of the thermal oceanic front on the Marine Atmospheric
Boundary Layer (MABL), in the BrazilMalvinas Confluence (BMC)
region, were studied. This was based in two cases of SST thermal
gradient intensities. One was more intense and the other less
intense. Both cases were studied under two different atmospheric
conditions. Using highresolution numerical model, we simulate and
analyzed the dynamic and thermodynamics of it, over two
orientations transects. One was perpendicular and the other
parallel to the SST thermal orientation gradient. The main
objective of this study was to analyze on which conditions the
mechanisms of vertical mixing and pressure adjustment occur in
MABL. Through of the terms of the momentum equation and heat
fluxes, it was observed that the mechanisms of pressure adjustment
and vertical mixing coexist under the two synoptic conditions
analyzed and operate in different ways on one side and the other
of the SST front. Under the presence of an atmospheric high
pressure system the MABL is locally modulated by the SST and
responds to the forcing, in which the minor order terms of the
trend equation can be neglected, since it is a quasigeostrophic
situation. On the other hand, under the influence of a low
atmospheric pressure system MABL is influenced by dynamic
mechanisms, which terms of friction and advection are in the same
order of pressure gradient force.",
committee = "Arav{\'e}quia, Jos{\'e} Antonio (presidente) and Pezzi, Luciano
Ponzi (orientador) and Lorenzzetti, Jo{\~a}o Ant{\^o}nio and
Camargo, Ricardo de and Polito, Paulo Simionato",
englishtitle = "Stability of the Marine Atmospheric Boundary Layer over
Brazil-Malvinas Confluence region",
language = "pt",
pages = "142",
ibi = "8JMKD3MGP3W34P/3Q5AEPH",
url = "http://urlib.net/ibi/8JMKD3MGP3W34P/3Q5AEPH",
targetfile = "publicacao.pdf",
urlaccessdate = "27 abr. 2024"
}