@Article{MendesTrigCavaDaCa:2008:ImClAd,
author = "Mendes, Monica Cristina Dami{\~a}o and Trigo, Ricardo Machado and
Cavalcanti, Iracema Fonseca Albuquerque and DaCamara, Carlos C.",
affiliation = "Univ Lusofona, Dept Engn, Lisbon, Portugal and Univ Lusofona, Dept
Engn, Lisbon, Portugal and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and Univ Lisbon, IDL, CGUL, P-1699 Lisbon,
Portugal",
title = "Blocking Episodes in the Southern Hemisphere: Impact on the
Climate of Adjacent Continental Areas",
journal = "Revista Brasileira de Geof{\'{\i}}sica",
year = "2008",
volume = "165",
number = "9-10",
pages = "1941--1962",
month = "oct.",
keywords = "blocking, southern hemisphere, South America, pacific ocean,
temperaturem precipitation.",
abstract = "This work presents an updated climatology of blocking episodes for
the Southern Hemisphere between 1960 and 2000, based on data from
NCEP/NCAR reanalysis. Five contiguous areas of blocking activity
are considered; Southeastern Pacific, Southwestern Pacific,
Atlantic, Indian and Oceania. The impact of the three most
important areas of onset blocking episodes (Southeastern Pacific,
Atlantic and Oceania) upon the climate of the adjacent continental
areas (South America and Australia) was evaluated. Composites of
the meteorological variables (temperature and precipitation) were
obtained for periods of diagnosed blockings. The impact of the
blocking episodes over the climate of South America and Australia
is highlighted whenever anomaly fields of temperature and
precipitation are significant at the 5% and 10% levels,
respectively. Impacts of Southeastern Pacific and Atlantic
blockings are observed on the temperature field over several
regions of South America. Significantly higher (lower)
temperatures than climatology occur in southern Brazil, northern
Argentina, Uruguay and Paraguay, and lower (higher) than
climatology in the extreme south of South America for the
Southeastern Pacific (Atlantic) blocking episodes. Precipitation
over South America is also affected by the Southeastern Pacific
and Atlantic blockings in different ways. The Southeastern Pacific
blocking has higher impact on precipitation in summer (dry
conditions in northeast Brazil) and spring (wet conditions in
central and southern Brazil), while the Atlantic blocking affects
precipitation in autumn and winter (wet conditions in parts of
central and southern Brazil). The blocking cases over Oceania
affect southeastern Australia with normal to higher than
climatological precipitation and with negative temperature
anomalies in that region. Finally we provide a detailed analysis
of a South Atlantic blocking episode, which occurred between the
4(th) and the 8(th) of June 1997. This event shows clearly the
split of the jet stream into two branches (subtropical and polar)
surrounding the anticyclonic sector, and satellite imagery
revealed the presence of transient systems in the periphery of the
blocking anticyclone responsible for high values of precipitation
in the southeastern sector of South America.",
doi = "10.1007/s00024-008-0409-4",
url = "http://dx.doi.org/10.1007/s00024-008-0409-4",
issn = "0102-261X",
language = "en",
targetfile = "Iracema_blocking.pdf",
urlaccessdate = "23 abr. 2024"
}