@Article{MendesCava:2014:ReThAn,
author = "Mendes, Monica Cristina Dami{\~a}o and Cavalcanti, Iracema
Fonseca de Albuquerque",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)}",
title = "The relationship between the antarctic oscillation and blocking
events over the south pacific and atlantic oceans",
journal = "International Journal of Climatology",
year = "2014",
volume = "34",
keywords = "blocking events, Antarctic Oscillation, southern hemisphere.",
abstract = "It is known that blocking events have impacts on the behaviour of
transient systems and affect the weather in southern continental
regions of the Southern Hemisphere. Since the main mode of
variability in Southern Hemisphere, the annular mode, or Antarctic
Oscillation (AAO), changes the extratropical atmospheric
circulation, the blocking characteristics over Pacific and
Atlantic Oceans are analysed in this study, in terms of the two
opposing phases of the AAO. The characteristics of atmospheric
flow patterns and blocking events are analysed as a function of
season during the period 1979-2000. The relative frequency of
blocked days is different for each AAO phase. Maximum duration and
number of events over the Southwestern Pacific and South Atlantic
regions occur in the positive phase, while the blocking activity
over the Southeastern Pacific region is similar in the two phases
but the persistence is higher in the negative phase. The
atmospheric anomalous centres associated with middle latitude and
polar AAO signals, as well as the behaviour of subtropical and
polar jets are discussed in relation to the blocking
characteristics. Convection over South America is analysed for
blocking periods in each AAO phase and is discussed based on
anomalous circulation in each phase. Wavetrain patterns over the
South Pacific and variations in intensity of jet streams induce
anomalous circulation over South America, which are associated
with the track and persistence of transient systems over
Southeastern South America and with convection over the
continent.",
doi = "10.1002/joc.3729",
url = "http://dx.doi.org/10.1002/joc.3729",
issn = "0899-8418",
label = "scopus 2013-11",
language = "en",
urlaccessdate = "27 abr. 2024"
}