@Article{BritoOyam:2014:DaCyPr,
author = "Brito, Sheila Santana de Barros and Oyama, Marcos Daisuke",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
de Aeron{\'a}utica e Espa{\c{c}}o (IAE)}",
title = "Daily cycle of precipitation over the northern coast of Brazil",
journal = "Journal of Applied Meteorology and Climatology",
year = "2014",
volume = "53",
number = "11",
pages = "2481--2502",
month = "Nov.",
keywords = "Climatology, Meteorology, Coastal meteorologies, Coefficient of
variation, Convective systems, Environmental conditions,
Meso-scale systems, Phase propagation, Physical mechanism,
Tropical rainfall measuring missions, Rain, climatology, coastal
zone, convective system, environmental conditions, marine
atmosphere, mesoscale meteorology, precipitation assessment, TRMM,
Brazil.",
abstract = "The daily cycle of precipitation (DCP) in the austral autumn on
the northern coast of Brazil (NCB) is examined in detail. The
Tropical Rainfall Measuring Mission 3B42 dataset was used to
obtain the DCP, and the intradaily variability was measured using
the coefficient of variation (CV). The DCP data of the NCB were
grouped into five regimes. A new regime was found, called the
shore regime. It has a minimum CV, and its cycle shows both
continental (late afternoon peak) and oceanic features (morning
peak). The landside coastal regime was divided into two areas: a
continental coast regime, with very high CV, and an inland coast
regime, with clear inland phase propagation. The continental
regime was divided into two categories: an inland regime with low
and high variability. The Forecast and Tracking of the Evolution
of Cloud Clusters (ForTraCC) data were used to relate convective
systems (CS) and their processes to the DCP. The following
processes are studied for the CS: initiation/dissipation,
merge/split, area increase/reduction, and advection. Initiation is
more concentrated in time, while dissipation is more distributed.
Physical mechanisms that generate initiation can promote area
expansion and hence CS merge. By considering a simple
parameterization, the time scale of the CS area reduction under
environmental conditions that are unfavorable to initiation ranges
from 6 to 12 h. Therefore, there is upscaling of the CS in the
afternoon and slow decay during the night and morning, which leads
to a more uniform cycle inland.",
doi = "10.1175/JAMC-D-14-0029.1",
url = "http://dx.doi.org/10.1175/JAMC-D-14-0029.1",
issn = "1558-8432 and 1558-8424",
label = "scopus 2015-01 BarrosBritoOyam:2014:DaCyPr",
language = "en",
urlaccessdate = "27 abr. 2024"
}