@Article{KayanoKous:1996:TrCiVa,
author = "Kayano, Mary Toshie and Kousky, Vernon E.",
affiliation = "Instituto Nacional de Pesquisas Espaciais (INPE), Centro de
Previs{\~a}o de Tempo e Estudos Clim{\'a}ticos (CPTEC) and
National Centers for Environmental Prediction, Climate Prediction
Center",
title = "Tropical circulation variability with emphasis on interannual and
intraseasonal time scales",
journal = "Revista Brasileira de Meteorologia",
year = "1996",
volume = "11",
number = "1 e 2",
pages = "06 -17",
month = "Jun.",
keywords = "tropical, circulation variability, emphasis, interannual,
intraseasonal.",
abstract = "Tropical atmosphere variability is analyzed by computing the
variance (total, interannual-IA, and intraseasonal-IS) of outgoing
longwave radiation (OLR), sea levei pressure (SLP), 250-hPa
streamfunction and 250-hPa velocity po- tential, and the percent
of total variance in the IA and IS bands, for the period 1985-1994
for ali seasons and for the austral summer and winter seasons,
separately. High OLR variability in the tropics and subtropics is
mainly associated with the IS band, whereas the maximum IA
variance observed in the equatorial central and eastern Pacific is
related to the EI Nirio-Southern Os- cillation (ENSO). The SLP
variance is largest in the extratropics, however, the pattern of
percent of total variance in the IA band shows maxima in the
tropics consistent with the centers of action of the Southern
Oscillation (SO). A substantial portion of the IS variance in SLP
is related to the Madden- Julian oscillation. The greatest
variance of the 250-hPa streamfunction is found in the subtropics
and lower midlatitudes. The small regions in the tropics with more
than 30% of the total variance in the IA band, during the austral
summer correspond to the main anomalous ENSO-related circulation
centers. The 250-hPa velocity potential shows maxima in total and
IS variance centered in the tropics. The IA variance is generally
quite small, except over Indonesia and the eastem tropical
Pacific, consistent with ENSO-re- lated anomalies. Seasonality is
evident in the variance patterns for ali variables. Maximum
variability is observed in the winter hemisphere for SLP and
250-hPa streamfunction and during the austral summer for OLR and
250- hPa velocity potential.",
copyholder = "SID/SCD",
issn = "0102-7786",
language = "en",
targetfile = "Kayano.Tropical.pdf",
urlaccessdate = "10 maio 2024"
}