@InProceedings{NobreMareCavaObre:2004:SePrPr,
author = "Nobre, Paulo and Marengo, Jose Antonio and Cavalcanti, Iracema
Fonseca de Albuquerque and Obregon, Guilhermo",
affiliation = "Instituto Nacional de Pesquisas Espaciais, Centro de Previs{\~a}o
do Tempo e Estudos Clim{\'a}ticos (INPE.CPTEC) and {UBA -
Argentina} and FUNCEME",
title = "Seasonal-to-decadal predictability and prediction of South
American climate",
year = "2004",
pages = "42",
organization = "CLIVAR Workshop on Atlantic Predictability.",
abstract = "South America represents an interesting area concerning seasonal
to interannual and longer climate variability. The largest
fraction of the continent is within the tropics, where seasonal
climate predictability is higher, if compared to mid latitudes,
and thus can benefit a large number of people. Also, it
encompasses a few important elements of the climate system, like
the Amazon rainforest, which covers a considerable fraction of the
continental area and represents an important source of upper level
mass and heat at lower latitudes; thus contributing both to the
general circulation of the atmosphere and to the local climate
(Buchmann et al., 1995). It is also subject to and interferes in
two convergence zones: the Intertropical Convergence Zone (ITCZ)
and the South Atlantic Convergence Zone (SACZ). The ITCZ is
modulated by surface features, like the interhemispheric gradient
of Sea Surface Temperature (SST) anomalies over the equatorial
Atlantic (Hastenrath and Druyan, 1993; Wagner, 1996; Chang et al.,
2000), and it modulates interannual variability of seasonal
rainfall over eastern Amazon and northern Nordeste (Hastenrath and
Heller, 1977; Moura and Shukla, 1981; Nobre and Shukla, 1996).
Atmospheric general circulation models (AGCM) simulate seasonal
rainfall interannual variability over Nordeste strikingly well
when observed global tropics SST are prescribed (Goddard and
Mason, 2002; Marengo et al., 2003). The SACZ, on the other hand,
is also influenced by SST anomalies over the southwestern tropical
Atlantic, has a strong impact on the rainfall regime over southern
Nordeste, Southeast and Southern Brazil, and contributes to
modulate underlying SSTs over the SW tropical Atlantic (Chaves and
Nobre, 2004). Differently from the ITCZ, however, the SACZ is
observed predominantly over negative SSTA (Robertson and Mechoso,
2000), suggesting that an atmospheric-forcing coupling is
operative at zero lag. AGCM experiments using direct SST thermal
forcing generates simulations with near zero or even negative
skill simulating SACZ (i.e., rainfall) variability (Marengo et
al., 2003). The high reproducibility of Nordeste, and to some
extent over southern Brazil, seasonal rainfall by AGCMs contrasts
with the low reproducibility of seasonal rainfall over
southeastern Brazil, indicating that different processes shall be
operating to modulate seasonal rainfall over those regions.",
conference-location = "Reading",
conference-year = "19-23 Apr.",
copyholder = "SID/SCD",
language = "en",
targetfile = "Nobre_Seasonal_to_decadal.pdf",
urlaccessdate = "29 jun. 2024"
}