@InProceedings{Chaves:2006:ObAn,
author = "Chaves, Rosane Rodrigues",
affiliation = "{Universidade Estadual do Norte Fluminense Darcy Ribeiro - UENF}
and {Laborat{\'o}rio de Engenharia e Explora{\c{c}}{\~a}o de
Petr{\'o}leo - LENEP} and {Laborat{\'o}rio de Meteorologia -
LAMET}",
title = "Patterns of sea surface temperature anomalies over north atlantic
ocean and convection over south america - observational analysis",
booktitle = "Proceedings...",
year = "2006",
editor = "Vera, Carolina and Nobre, Carlos",
pages = "995--997",
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 = "SST, North Atlantic, South America, summertime convection.",
abstract = "Patterns of sea surface temperature (SST) anomalies over North
Atlantic (Equator - 40ºN and 70ºW - 0º) are determined by
Principal Components Analysis (PCA) to December-January-February
(DJF) from 1979 to 2001. Association of these patterns with
summertime convection over South America is determined by linear
correlation between the time series of these patterns and Outgoing
Longwave Radiation (OLR) anomalies over this continent. Coupled
modes between North Atlantic SST anomalies and OLR anomalies over
South America (40ºS-20ºN to 90ºW-20ºW) are determined by SVD also
to DJF from 1979 to 2001. The spatial pattern associated with the
first anomalies SST mode determined by (PCA) shows one monopolo
pattern. The second pattern shows an out-of-phase relationship
between SST anomalies over tropical and subtropical region. The
third pattern shows three action centers over Atlantic North, SST
anomalies with same signal over equatorial and subtropical region
and different signal over intermediate region. The first and third
patterns show greater interannual variability and the second
pattern interdecadal variability. The first and second pattern
does not show correlation significant with summertime convection
over South America. The third pattern shows correlation
significant with summertime convection only over northern of South
America. The convection in this region is associated with positive
SST anomalies over equatorial and subtropical region and negative
SST over tropical region. The first coupled mode between SST
anomalies over North Atlantic and OLR anomalies over South America
determined by SVD corresponds to the third mode of the SST
anomalies over North Atlantic determined by PCA. Thus, apparently,
third mode of the SST anomalies over North Atlantic ((Equator -
40ºN and 70ºW - 0º) has greater influence over summertime
convection over South America than the two first modes. Results
indicate also that North Atlantic (Equator - 40ºN and 70ºW - 0º)
SST has influence only in the summertime convection over northern
South America.",
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/2005/10.31.15.33",
url = "http://urlib.net/ibi/cptec.inpe.br/adm_conf/2005/10.31.15.33",
targetfile = "995-997.pdf",
type = "Monsoon systems and continental rainfall",
urlaccessdate = "11 maio 2024"
}