@Article{RossatoSouz:2016:ObSoMo,
author = "Rossato, Fernando and Souza, Ronald Buss de",
affiliation = "{Universidade Federal de Santa Maria (UFSM)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)}",
title = "Observa{\c{c}}{\~o}es sobre a modula{\c{c}}{\~a}o da camada
limite atmosf{\'e}rica marinha devida {\`a} passagem de um
sistema frontal no Atl{\^a}ntico Sudoeste",
journal = "Ci{\^e}ncia e Natura",
year = "2016",
volume = "38",
number = "Esp.",
pages = "388--293",
note = "{IX Workshop Brasileiro de Micrometerologia}",
keywords = "Camada Limite Atmosf{\'e}rica Marinha. Fluxos de calor, Marine
Atmospheric Boundary Layer. Heat Fluxes.",
abstract = "Entre os dias 6 a 9 de dezembro de 2012, o Navio
Oceanogr{\'a}fico Alpha-Crucis realizou esta{\c{c}}{\~o}es
oceanogr{\'a}ficas no Oceano Atl{\^a}ntico Sudoeste em apoio aos
projetos SAMOC e ACEx. Durante o cruzeiro de pesquisa, o navio
realizou medi{\c{c}}{\~o}es com o lan{\c{c}}amento de
bal{\~o}es meteorol{\'o}gicos. A partir de dados coletados pelas
radiossondas, foi poss{\'{\i}}vel verificar a variabilidade da
camada limite atmosf{\'e}rica marinha (CLAM) na {\'a}rea e
per{\'{\i}}odo de estudo. A partir de dados meteorol{\'o}gicos
e oceanogr{\'a}ficos, foi poss{\'{\i}}vel estimar os fluxos de
calor latente e sens{\'{\i}}vel a partir de
parametriza{\c{c}}{\~o}es bulk. Durante um epis{\'o}dio de
forma{\c{c}}{\~a}o de um ciclone extratropical, os resultados
desse trabalho demonstram o impacto das condi{\c{c}}{\~o}es
sin{\'o}ticas sobre a evolu{\c{c}}{\~a}o da CLAM. Na
condi{\c{c}}{\~a}o pr{\'e}-frontal, verificou-se uma
estratifica{\c{c}}{\~a}o da CLAM. Os fluxos de calor latente e
sens{\'{\i}}vel dirigidos do oceano para a atmosfera foram
baixos ou negativos (da atmosfera para o oceano). Na
condi{\c{c}}{\~a}o p{\'o}s-frontal, a CLAM apresentou-se bem
desenvolvida, com uma altura de 1200 m e os fluxos de calor
latente e sens{\'{\i}}vel do oceano para a atmosfera foram mais
intensos. Essas observa{\c{c}}{\~o}es s{\~a}o fundamentais para
ampliar o entendimento dos processos f{\'{\i}}sicos que ocorrem
na interface oceano-atmosfera e tem import{\^a}ncia prim{\'a}ria
para a previs{\~a}o do tempo e clima na regi{\~a}o sul-sudeste
do Brasil. ABSTRACT: Between 6-9 December 2012, the Oceanographic
Vessel Alpha Crucis took oceanographic stations in the
Southwestern Atlantic Ocean in support to both SAMOC and ACEx
projects. During the research cruise, the vessel performed
measurements with the release of weather balloons. From the data
collected by the radiosondes, it was possible to verify the
variability of the marine atmospheric boundary layer (MABL) in the
area and period of study. From meteorological and oceanographic
data, it was possible to estimate the latent and sensible heat
fluxes from bulk parameterization. During an episode of formation
of an extratropical cyclone, the results ,of this work demonstrate
the impact of the synoptic conditions influencing the evolution of
the MABL. During the prefrontal condition a stratification of the
MABL was verified. The latent and sensible heat fluxes directed
from the ocean to the atmosphere were low or negative (from the
atmosphere to the ocean). During the post frontal condition, the
MABL was well developed with a 1200 m height and the latent and
sensible heat fluxes from the ocean to the atmosphere were more
intense. These observations are fundamental to widen our
understanding on the physical processes occurring at the
ocean-atmosphere interface and have primary importance for the
weather and climate forecast of the south-southwestern region of
Brazil.",
doi = "10.5902/2179460X20278",
url = "http://dx.doi.org/10.5902/2179460X20278",
issn = "0100-8307 and 2179-460X",
language = "pt",
targetfile = "Rossato_observacoes.pdf",
url = "http://periodicos.ufsm.br/cienciaenatura/article/view/20278/pdf",
urlaccessdate = "11 maio 2024"
}