@Article{BarrosOyam:2010:SiMeAs,
author = "Barros, Sheila Santana de and Oyama, Marcos Daisuke",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
de Aeron{\'a}utica e Espa{\c{c}}o (IAE)}",
title = "Sistemas meteorol{\'o}gicos associados {\`a} ocorr{\^e}ncia de
precipita{\c{c}}{\~a}o no centro de lan{\c{c}}amento de
Alc{\^a}ntara",
journal = "Revista Brasileira de Meteorologia",
year = "2010",
volume = "25",
number = "3",
pages = "333--344",
keywords = "chuva, sistemas convectivos, costa norte do Brasil, rainfall,
convective systems, Brazilian northern coast.",
abstract = "O Centro de Lan{\c{c}}amento de Alc{\^a}ntara (CLA; 2° 22'S, 44º
23'W) tem papel importante para as atividades aeroespaciais no
Brasil, sendo de interesse estudar os sistemas precipitantes
atuantes sobre a regi{\~a}o. O trabalho teve como objetivo
caracterizar os sistemas associados aos eventos de
precipita{\c{c}}{\~a}o ocorridos no CLA entre 2005 e 2006,
utilizando totais hor{\'a}rios de precipita{\c{c}}{\~a}o, dados
de Rean{\'a}lise do NCEP/NCAR, temperatura de brilho do
sat{\'e}lite GOES-12 e radia{\c{c}}{\~a}o de onda longa
emergente. Para tal, definiram-se crit{\'e}rios para identificar
os sistemas meteorol{\'o}gicos de grande, meso e de escala local
associados {\`a} precipita{\c{c}}{\~a}o no CLA. Os resultados
apontaram que 40% dos eventos de precipita{\c{c}}{\~a}o
estiveram associados a fatores de grande escala, destacando-se a
Zona de Converg{\^e}ncia Intertropical. Verificou-se que 60%
(40%) dos eventos de precipita{\c{c}}{\~a}o se devem a processos
estratiformes (convectivos). Os sistemas convectivos apresentaram
as seguintes caracter{\'{\i}}sticas: {\'a}reas entre 104 km2 e
25x104 km2, chuva posicionada na por{\c{c}}{\~a}o convectiva do
sistema, intensifica{\c{c}}{\~a}o por convec{\c{c}}{\~a}o
diurna, inclus{\~a}o em um sistema de escala maior e origem
preferencial de sudeste ou nordeste. Os sistemas formados por
processos estratiformes se subdividiram quase igualmente em dois
grupos: resqu{\'{\i}}cios de sistemas convectivos anteriormente
atuantes no CLA e sistemas que n{\~a}o est{\~a}o associados a
nenhum processo convectivo. ABSTRACT: The Alc{\^a}ntara Rocket
Launching Center (CLA; 2° 22'S, 44º 23'W) plays an important role
in aerospace research activities in Brazil, and so it is of
interest to study the precipitation systems over the CLA region.
This work aimed at characterizing the systems associated with
precipitation occurrence at CLA from 2005 to 2006 by using hourly
precipitation data, NCEP/NCAR Reanalysis data, brightness
temperature data from GOES-12 satellite and outgoing longwave
radiation data. Criteria were defined to identify large, meso and
local scale meteorological systems associated with precipitation
at CLA. About 40% of precipitation events were associated with
large scale systems, mainly the Intertropical Convergence Zone,
and about 60% (40%) of precipitation events are due to convective
(stratiform) processes. The convective systems showed the
following characteristics: area between 104 km2 e 25x104 km2,
precipitation located in convective part of the system,
intensification by diurnal convection, inclusion in a larger scale
system and preferred southeasterly or northeasterly propagation.
The systems formed from stratiform processes could be divided
almost equally in two groups: reminder of convective systems
previously active over CLA and systems that are not associated
with any convective process.",
doi = "10.1590/S0102-77862010000300005",
url = "http://dx.doi.org/10.1590/S0102-77862010000300005",
issn = "0102-7786",
language = "pt",
targetfile = "barros.pdf",
urlaccessdate = "15 jun. 2024"
}