@Article{MarengoCKAPSSLSBCGBT:2012:ClReAn,
author = "Marengo, Jose Antonio and Chou, SC and Kay, Gillian and Alves,
Lincoln M. and Pesquero, Jose and Soares, Wagner and Santos,
Daniel C. and Lyra, Andre and Sueiro, Gustavo and Betts, Richard
and Chagas, Diego and Gomes, J and Bustamente, Josiane and
Tavares, Priscila",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and UK Met Off Hadley Ctr,
Exeter EX1 3PB, Devon, England. and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {Instituto Nacional de Pesquisas Espaciais (INPE)} and
{} and {} and UK Met Off Hadley Ctr, Exeter EX1 3PB, Devon,
England.",
title = "Development of regional future climate change scenarios in South
America using the Eta CPTEC/HadCM3 climate change projections:
climatology and regional analyses for the Amazon, S{\~a}o
Francisco and the Parana River basins",
journal = "Climate Dynamics",
year = "2012",
volume = "38",
number = "9-10",
pages = "1829--1848",
keywords = "South America, climate change, downscaling, Amazon region.",
abstract = "The objective of this study is to assess the climate projections
over South America using the Eta-CPTEC regional model driven by
four members of an ensemble of the Met Office Hadley Centre Global
Coupled climate model HadCM3. The global model ensemble was run
over the twenty-first century according to the SRES A1B emissions
scenario, but with each member having a different climate
sensitivity. The four members selected to drive the Eta-CPTEC
model span the sensitivity range in the global model ensemble. The
Eta-CPTEC model nested in these lateral boundary conditions was
configured with a 40-km grid size and was run over 1961-1990 to
represent baseline climate, and 2011-2100 to simulate possible
future changes. Results presented here focus on austral summer and
winter climate of 2011-2040, 2041-2070 and 2071-2100 periods, for
South America and for three major river basins in Brazil.
Projections of changes in upper and low-level circulation and the
mean sea level pressure (SLP) fields simulate a pattern of
weakening of the tropical circulation and strengthening of the
subtropical circulation, marked by intensification at the surface
of the Chaco Low and the subtropical highs. Strong warming (4-6°C)
of continental South America increases the temperature gradient
between continental South America and the South Atlantic. This
leads to stronger SLP gradients between continent and oceans, and
to changes in moisture transport and rainfall. Large rainfall
reductions are simulated in Amazonia and Northeast Brazil
(reaching up to 40%), and rainfall increases around the northern
coast of Peru and Ecuador and in southeastern South America,
reaching up to 30% in northern Argentina. All changes are more
intense after 2040. The Precipitation-Evaporation (P-E) difference
in the A1B downscaled scenario suggest water deficits and river
runoff reductions in the eastern Amazon and S{\~a}o Francisco
Basin, making these regions susceptible to drier conditions and
droughts in the future.",
doi = "10.1007/s00382-011-1155-5",
url = "http://dx.doi.org/10.1007/s00382-011-1155-5",
issn = "0930-7575",
label = "lattes: 5719239270509869 1 OrsiniCKAPSSLSRCGBT:2011:ClAnRe",
language = "en",
targetfile = "Orsini-Climate Dyn-fulltext[1].pdf",
urlaccessdate = "18 abr. 2024"
}