@InProceedings{CavalcantiChouGome:2013:FlSoBr,
author = "Cavalcanti, Fonseca de Albuquerque and Chou, Sin Chan and Gomes,
Jorge Luis",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)}",
title = "Floods in Southeastern Brazil- Observations, Simulation,
Projection and Uncertainties",
booktitle = "Abstracts...",
year = "2013",
organization = "European Conference on Severe Storms, 7. (ECSS).",
keywords = "floods, Brazil, satellite images, precipitation.",
abstract = "Cases of floods in Southeastern Brazil are analyzed, discussing
the associated synoptic features and the convection in the systems
shown in satellite images. Cases of heavy precipitation in this
region are identified in a climate simulation of present time and
in a climate projection under global warming using the Regional
Eta Model. The synoptic and mesoscale conditions, associated with
heavy precipitation, simulated by the model are analyzed. The
frequencies and intensities of extreme precipitation cases are
obtained from four members of the simulations and projections, and
an uncertainty analysis is performed with the results. One of the
extreme precipitation cases is illustrated: the case that happened
in Southeastern Brazil (Rio de Janeiro) from 31st December 2009 to
1st January 2010. There were several landslides in the region, one
of which destroyed a beach hotel killing many people. The
satellite image showed the influence of several synoptic systems
in the region, as the Bolivian High displaced from its normal
position, the upper level cyclonic vortex close to Northeastern
Brazil coast and a frontal system extending from the region
towards the ocean. The synoptic condition, with low level wind
confluence over the region, high relative humidity above 80% and
strong divergence at high levels favored by the displacement of
the Bolivian High southeastward contributed to the heavy
precipitation associated with the oceanic squall line embedded in
the frontal system. A simulation of this case with high resolution
of Eta Model shows the ability of the model in representing the
extreme precipitation.",
conference-location = "Helsinki",
conference-year = "3-7 junho 2013",
label = "self-archiving-INPE-MCTI-GOV-BR",
language = "en",
targetfile = "cavalcanti_floods.pdf",
urlaccessdate = "08 maio 2024"
}