@InProceedings{SouzaRoch:2006:DiVaRa,
author = "Souza, Everaldo B. De and Rocha, Edson J. P. Da",
affiliation = "Divis{\~a}o de Meteorologia, SIPAM/ATECH, Manaus-AM, Brasil and
Departamento de Meteorologia, UFPa, Bel{\'e}m-PA, Brasil",
title = "On the diurnal variability of rainfall in eastern amazonia along
atlantic coast during rainy season",
booktitle = "Proceedings...",
year = "2006",
editor = "Vera, Carolina and Nobre, Carlos",
pages = "1203--1207",
organization = "International Conference on Southern Hemisphere Meteorology and
Oceanography, 8. (ICSHMO).",
publisher = "American Meteorological Society (AMS)",
address = "45 Beacon Hill Road, Boston, MA, USA",
keywords = "eastern Amazonia, diurnal cycle, precipitation, ITCZ.",
abstract = "The knowledge of variation of precipitation over short timescales,
such as the diurnal cycle, is essential in understanding of the
physics of tropical atmosphere. The diurnal variability of
rainfall in particular over the Amazonia has been previously
documented using high temporal resolution data collected in field
experiments, like ABRACOS (Anglo Brazilian Climate Observation
Study) and LBA (Large-scale Biosphere-Atmosphere Experiment in
Amazonia). Previous works that used these data evidenced rainfall
maxima in southwest and central Amazonia (Ji-Paran{\'a} and
Manaus) in late afternoon, while in eastern Amazonia (Marab{\'a})
there is a maximum in the morning. On the other hand, there have
been few investigations on the diurnal variability of rainfall in
particular over eastern Amazonia along Atlantic coast. In the
present work, five years (2001-2005) of continuous rainfall data
collected by Mil{\^e}nioLBA (Large-scale Biosphere-Atmosphere
Experiment in Amazonia) station in Bragan{\c{c}}a (00º 50' S, 46º
38' W) are used in order to describe coherent diurnal variation of
rainfall in eastern Amazonia off Atlantic coast during rainy
season (January to May). The 5-yr average of accumulation of
rainfall in each 6 h (06:00, 12:00, 18:00 and 24:00 LST) evidenced
a maximum peak during morning and a sharp minimum in the
afternoon. A significant diurnal cycle related to Intertropical
Convergence Zone activity in the equatorial Atlantic is pointed
out as the main mechanism regulator of diurnal pluviometric
variability in coastal region along Par{\'a} and Amap{\'a}
states. March presents highest frequency of rainy days following
by April and February. Furthermore, the frequency distribution of
rainfall considering different intensity ranges (0.1 to 5, 5.1 to
10, 10.1 to 25, 25.1 to 50, 50.1 to 75, 75.1 to 100 and > 100 mm)
is documented for each month and period of diurnal cycle. An
outstanding result evidenced is frequency distribution of events
with rainfall less than 5 mm, which explain the largest
proportional contribution of the rainfall total observed during
rainy season that reach 21.6% in January, 24.5% in May, 29.8% in
February, 33.2% in April and 36% in March.",
conference-location = "Foz do Igua{\c{c}}u",
conference-year = "24-28 Apr. 2006",
language = "en",
organisation = "American Meteorological Society (AMS)",
ibi = "cptec.inpe.br/adm_conf/2005/10.30.19.43",
url = "http://urlib.net/ibi/cptec.inpe.br/adm_conf/2005/10.30.19.43",
targetfile = "1203-1208.pdf",
type = "Monsoon systems and continental rainfall",
urlaccessdate = "02 maio 2024"
}