%0 Journal Article
%4 dpi.inpe.br/plutao/2012/11.28.18.29.58
%2 dpi.inpe.br/plutao/2012/11.28.18.29.59
%@doi 10.4236/ajcc.2012.13011
%@issn 2167-9495
%@issn 2167-9509
%F lattes: 6731029375224939 1 Cavalcanti:2012:ClFiOv
%T Climate Fields over South America and Variability of SACZ and PSA in HadGEM2-ES CMIP5
%D 2012
%8 Set.
%A Cavalcanti, Iracema Fonseca de Albuquerque,
%A Shimizu, Marilia Harumi,
%@affiliation Instituto Nacional de Pesquisas Espaciais (INPE)
%@affiliation Instituto Nacional de Pesquisas Espaciais (INPE)
%@electronicmailaddress iracema@cptec.inpe.br
%B American Journal of Climate Change
%V 1
%N 3
%P 132-144
%K South America Precipitation, HadGEM2-ES, Model Simulation, Model Projections, SACZ, PSA.
%X Historical simulations (present climate) and projections under RCP8.5 scenario (future climate) by HadGEM2-ES of temperature and precipitation are analyzed during the four seasons in South America. Projections of precipitation are discussed in terms of atmospheric circulation. The South Atlantic Convergence Zone (SACZ) and the Pacific South America (PSA) patterns are analyzed in simulations of present climate and in future climate projections. The model shows small systematic errors over South America, larger close to the northern South American coast in DJF and MAM. The seasonal variability of precipitation, temperature and wind fields is very well reproduced, mainly the summer/winter differences. The SACZ and the Intertropical Convergence Zone (ITCZ) are well simulated. The good model performance to reproduce the precipitation, temperature and wind fields, in the present climate, gives confidence in the projection results subject to the future scenarios. Changes from the present time to the future indicate increased precipitation over southern and southeastern Brazil and areas nearby and the tropical western South American coast. Reduced precipitation is projected over eastern Amazonia, northern South America and southern Chile. The changes are related to changes in the low level wind flow over the tropical North Atlantic, which reduces the advection of moisture to the continent and also to the increased low level flow over central South America southwards, which increases the humidity in the southern regions. The upper level flow changes are also consistent with the precipitation changes. There is a weakening of the Bolivian High and a strengthening of the subtropical jet over the continent. The SACZ dipole pattern is well simulated and in the future projections the southern center anomalies are more intense than in the present time. The PSA1 and PSA2 patterns are well represented in the present climate, but in the future projection only one dominant mode is identified as the typical teleconnection over the Pacific and South America.
%@language en
%3 AJCC20120300003_76381802.pdf