@MastersThesis{Cabrera:2018:EsMeFí,
author = "Cabrera, Mylene Jaen",
title = "Estudo dos mecanismos f{\'{\i}}sicos respons{\'a}veis pela
estabilidade da camada limite atmosf{\'e}rica marinha na
regi{\~a}o do Atl{\^a}ntico Sudoeste",
school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
year = "2018",
address = "S{\~a}o Jos{\'e} dos Campos",
month = "2018-05-29",
keywords = "camada limite atmosf{\'e}rica marinha, atl{\^a}ntico sudoeste,
advec{\c{c}}{\~a}o de temperatura, modelo COAWST,
opera{\c{c}}{\~a}o ant{\'a}rtica XXXIII, marine atmospheric
boundary layer, southwest atlantic, temperature advection, coawst
model, antartic operation XXXIII.",
abstract = "Com o objetivo de estudar os mecanismos din{\^a}micos e
termodin{\^a}micos na interface oceano-atmosfera
respons{\'a}veis pela estabilidade da camada limite
atmosf{\'e}rica marinha (CLAM), na regi{\~a}o sudoeste do oceano
Atl{\^a}ntico Sul, este trabalho utilizou o sistema de modelagem
num{\'e}rica acoplado regional Coupled Ocean AtmosphereWave
Sediment Transport (COAWST), com alt{\'{\i}}ssima
resolu{\c{c}}{\~a}o espacial, e dados medidos in situ durante a
Opera{\c{c}}{\~a}o Ant{\'a}rtica XXXIII (OP33). As
simula{\c{c}}{\~o}es realizadas com o modelo COAWST foram
avaliadas considerando a temperatura da superf{\'{\i}}cie do mar
(TSM) e perfis verticais de temperatura e vento. No qual
verificou-se que o modelo reproduziu de forma acertada tanto a TSM
como os perfis de temperatura e vento. A estabilidade e o
desenvolvimento da CLAM foram analisados, considerando a
modula{\c{c}}{\~a}o local de TSM e os padr{\~o}es advectivos
impostos pelas condi{\c{c}}{\~o}es sin{\'o}ticas atuantes. Para
isso, foram selecionados tr{\^e}s estudos de caso, sob
influ{\^e}ncia de condi{\c{c}}{\~o}es pr{\'e}-frontais,
frontais e p{\'o}s-frontais. Os resultados demonstraram que a
CLAM foi modulada pela advec{\c{c}}{\~a}o t{\'e}rmica,
condicionada pelas situa{\c{c}}{\~o}es sin{\'o}ticas
atmosf{\'e}ricas analisadas e pela TSM local, assim como foi
observado em alguns casos um maior desenvolvimento da CLAM
associado com o incremento do vento em superf{\'{\i}}cie. Na
verifica{\c{c}}{\~a}o do mecanismo de ajuste hidrost{\'a}tico,
foi observado a atua{\c{c}}{\~a}o deste mecanismo no estudo de
caso influenciado por condi{\c{c}}{\~o}es frontais. A
an{\'a}lise do papel dos termos das equa{\c{c}}{\~o}es
horizontais de momentum em superf{\'{\i}}cie evidenciou maior
influ{\^e}ncia dos termos de gradiente de press{\~a}o, coriolis,
advec{\c{c}}{\~a}o e tend{\^e}ncia total, assim como, uma
rela{\c{c}}{\~a}o entre o aumento do termo de difus{\~a}o
horizontal e a diminui{\c{c}}{\~a}o do vento em
superf{\'{\i}}cie em dois dos tr{\^e}s casos analisados.
ABSTRACT: In order to study the dynamical and thermodynamic
mechanisms at the oceanatmosphere interface, responsible for the
stability of the Marine Atmospheric Boundary Layer (MABL), in the
southwest of the South Atlantic Ocean, this work used the regional
numerical modeling system Coupled Ocean Atmosphere Wave Sediment
Transport (COAWST), with very high spatial resolution, and data
measured in situ during Antarctic Operation XXXIII. The COAWST
model simulations were evaluated considering the Sea Surface
Temperature (SST) and temperature and wind vertical profiles. It
was verified that the model correctly reproduced both SST and
temperature and wind profiles. The MABL stability and development
were analyzed, considering the local modulation of the SST and
advective patterns imposed by synoptic conditions. Thus, three
case studies were selected, influenced by pre-frontal, frontal and
post-frontal conditions. The results showed that the MABL was
modulated by thermal advection, conditioned by atmospheric
synoptic conditions and local SST, as well as in some cases, a
greater MABL development was associated with surface wind
increment. During the case study influenced by frontal conditions,
the hydrostatic adjustment mechanism was observed. The horizontal
equation terms role analysis of the surface momentum showed a
greater influence of the pressure gradient, coriolis, advection
and total tendency, as well as a relation between the horizontal
diffusion term increase and the surface wind reduction in two of
three analyzed cases.",
committee = "Arav{\'e}quia, Jos{\'e} Antonio (presidente) and Pezzi, Luciano
Ponzi (orientador) and Camargo, Ricardo de",
englishtitle = "Physical mechanisms study responsible for the stability of the
marine atmospheric boundary layer in the Southwest Atlantic
region.",
language = "pt",
pages = "120",
ibi = "8JMKD3MGP3W34R/3R5MRN5",
url = "http://urlib.net/ibi/8JMKD3MGP3W34R/3R5MRN5",
targetfile = "publicacao.pdf",
urlaccessdate = "27 abr. 2024"
}