@MastersThesis{Dourado:1994:EsCaLi,
author = "Dourado, Marcelo Sandin",
title = "Estudo da camada limite planet{\'a}ria atmosf{\'e}rica
mar{\'{\i}}tima",
school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
year = "1994",
address = "Sao Jose dos Campos",
month = "1994-02-07",
keywords = "ci{\^e}ncias meteorol{\'o}gicas, Cabo Frio (RJ), camada limite,
atmosfera, meteorological science, boundary layer, atmosphere.",
abstract = "A evolu{\c{c}}{\~a}o temporal e espacial (vertical) da camada
limite planet{\'a}ria atmosf{\'e}rica mar{\'{\i}}tima em
regi{\~o}es subtropicais {\'e} investigada por meio de estudo
observacional e num{\'e}rico. Para tanto, foi realizada uma
campanha de medidas onde foram feitas sondagens simult{\^a}neas
do oceano e da atmosfera na regi{\~a}o de Cabo Frio (23.S e
42.08'W). Para o estudo num{\'e}rico foi utilizado um modelo de
fechamento de segunda ordem, proposto por Mellor e Yamada (1982),
acoplado a um modelo de camada de mistura oce{\^a}nica (CMO) para
determinar a temperatura da CMO em termos do balan{\c{c}}o de
energia. Embora a campanha de medidas tenha sido feita durante a
passagem de um sistema frontal, o que restringe a
utiliza{\c{c}}{\~a}o dos dados, compara{\c{c}}{\~o}es entre as
simula{\c{c}}{\~o}es e as observa{\c{c}}{\~o}es indicam que a
camada de mistura atmosf{\'e}rica simulada {\'e} consistente com
as observadas durante o experimento, bem como {\'e} similar
{\`a} observada por Fitzjarrald e Garstang (1981) durante o GATE.
Os perfis verticais simulados das vari{\^a}ncias das componentes
zonal, meridional e vertical da velocidade s{\~a}o
t{\'{\i}}picos de casos nos quais a for{\c{c}}ante
mec{\^a}nica {\'e} a principal respons{\'a}vel pela
forma{\c{c}}{\~a}o da camada de mistura (regime de
convec{\c{c}}{\~a}o for{\c{c}}ada). O aumento da temperatura da
camada de mistura oce{\^a}nica, simultaneamente ao aprofundamento
da CMO, est{\'a} associado {\`a} advec{\c{c}}{\~a}o de aguas
quentes da corrente do Brasil e costeiras. As
simula{\c{c}}{\~o}es da profundidade da CMO indicam que o
crescimento observado da CMO durante o experimento foi
intensificado pela subsid{\^e}ncia da Agua Central do
Atl{\^a}ntico Sul. ABSTRACT: The temporal and spatial (vertical)
evolution of the atmospheric marine boundary layer in subtropical
regions is investigated through observational and numerical
approaches. The observational part was done with field experiment
using simultaneous soundings from both atmosphere and ocean in the
Cabo Frio region ( 23º S e 42º08'W). The numerical study used a
second order closure model, as suggested by Mellor and Yamada
(1982), coupled to an oceanic mixing layer model (OML) in order to
determine the temperature of OML in terms of the energy balance.
Although the field experiment had been done under a frontal system
passage, what could create drawbacks in using those data,
comparing the imulations against observational it was found that
the simulated atmosphere boundary layer is consistent with the
observed one during the experiment; as well is similar to the
observed by Fitzjarrald and Garstang (1981) during the GATE. The
simulated vertical profiles of the zonal, meridional and vertical
components of the speed variance are typical from situations where
the mechanic forcing is the main cause of mixing layer formation
(forced convection). The increasing of temperature in the oceanic
mixing layer, simultaneously with the deepening of OML is
associated with the warm water advection, from the current of the
Brazil. The simulations of the OML during the experiment was
intensyfied due the subsidence of South Atlantic Central Warter
(SACW).",
committee = "S{\'a}, Leornardo Deane de Abreu (presidente) and Innocentini,
Valdir (orientador) and Stech, Jos{\'e} Luiz and Oliveira, Amauri
Pereira de and Moraes, Osvaldo Luis Leal",
copyholder = "SID/SCD",
englishtitle = "Study of the marine atmospheric boundary layer",
label = "6960",
language = "pt",
pages = "126",
ibi = "6qtX3pFwXQZ3r59YCT/GUfpo",
url = "http://urlib.net/ibi/6qtX3pFwXQZ3r59YCT/GUfpo",
targetfile = "publicacao.pdf",
urlaccessdate = "01 maio 2024"
}