@InProceedings{CavalcantiMare:2003:TyFeSo,
author = "Cavalcanti, Iracema Fonseca Albuquerque and Marengo, Jos{\'e}
Antonio",
affiliation = "Centro de Previs{\~a}o de Tempo e Estudos
Clim{\'a}ticos/Instituto Nacional de Pesquisas Espaciais,
Cachoeira Paulista, S{\~a}o Paulo",
title = "Typical features of the South America monsoon system, and
relations with the low level jet and South Atlantic convergence
zone in a climate AGCM simulation",
booktitle = "Proceedings...",
year = "2003",
pages = "70--71",
organization = "International Conference on Southern Hemisphere Meteorology and
Oceanography, 7.",
publisher = "American Meteorological Society",
keywords = "Meteorologia.",
abstract = "The main features of the South America Monsoon system are
simulated by the CPTEC/COLA AGCM in a climate ensemble simulation.
Results of nine integrations with T62L28 model resolution for the
period 1982-1991 are analysed in an ensemble mode and also
considering daily results of the individual members. Low and upper
levels wind fields in the summer season are typical and differ
completelly of those of the winter. In the summer the Bolivian
High and the Upper Atlantic Trough is well represented, as well as
the position of the Atlantic subtropical High which affects the
direction of the trade winds over the northeast brazilian coast.
Extreme cases of precipitation anomalies over South America in the
summer season are related to the behaviour of the main
characteristics of the monsoon. An opposite relation occur between
southeastern and southern Brazil during these extreme cases. The
anomalies are associated with the direction of the low level flow
from the Atlantic and Amazonia region, toward south, in the case
of dry southeast and wet south, and toward southeast, in the case
of dry south and wet southeast. It is seen, in these results, the
opposite relation between the South Atlantic Convergence Zone
(SACZ) and the Low Level Jet (LLJ) to the east of Andes. The
extreme cases occur in ENSO episodes, suggesting a large scale
influence on the South America Monsoon system. The overestimation
of the SACZ by the model is also consistent with a reduced number
of LLJ cases in the summer, when compared to the reanalyses
results. Although the model, in ENSO years and in the climatology,
represent well these features, in other years, the anomaly
precipitation over central and southeastern Brazil is poorly
simulated by the ensemble mean. The large dispersion among the
members and the different behaviour of the synoptic systems over
the region in each integration, give a low degree of
predictability for this region, in contrast to the northeastern
and the southern regions which have higher degree of
predictability. Individual analysis of the memberīs ensemble and
the behaviour of the monsoon system in each case are performed to
investigate the possibility of improvement in the seasonal
prediction of the region.",
conference-location = "Wellington, New Zealand",
conference-year = "24-28 Mar",
copyholder = "SID/SCD",
language = "en",
ibi = "x6e6X3pFwXQZ3DUS8rS5/yakET",
url = "http://urlib.net/ibi/x6e6X3pFwXQZ3DUS8rS5/yakET",
targetfile = "2003_cavalcanti.pdf",
type = "PRE",
url = "http://ams.confex.com/ams/pdfview.cgi?username=59611",
urlaccessdate = "29 jun. 2024"
}