@Article{VadlamudiFranFern:2000:CoBlOv,
author = "Vadlamudi, Brahmananda Rao and Franchito, Sergio Henrique and
Fernandez, Julio Pablo Reyes",
affiliation = "{Instituto Nacional de Pesquisas Espaciais}",
title = "Comments on blocking over the South Pacific and rossby wave
propagation",
journal = "Monthly Weather Review",
year = "2000",
volume = "128",
number = "12",
pages = "4160--4161",
month = "dec.",
keywords = "hemisphere, oscilation, variability.",
abstract = "In a recent study Renwick and Revell (1999, hereafter RR99)
investigated the atmospheric blocking over the South Pacific. They
found that the blocking events occur more frequently over the
southeast Pacific during El Nino events in austral spring. Their
analysis showed that blocking events are associated with
large-scale wave trains lying across the South Pacific from
Australia to southern South America. RR99 performed numerical
experiments with a linearized barotropic model and showed that the
tropical convective heating associated with OLR anomalies,
presumably generated during El Nino events, can generate similar
wave trains. The purposeof the present comment is to provide
observational evidence to show that the Rossby wave propagation
similar to the one noted by RR99 is in fact stronger and better
organized in austral spring than in other seasons.",
copyholder = "SID/SCD",
issn = "0027-0644",
language = "en",
targetfile = "Vadlamudi_Comments on blocking over the",
urlaccessdate = "04 maio 2024"
}