@InProceedings{MarengoSoarSaul:2002:ClLoJe,
author = "Marengo, Jos{\'e} Antonio and Soares, Wagner Rodrigues and Saulo,
Celeste",
affiliation = "Instituto Nacional de Pesquisas Espaciais, Centro de Previs{\~a}o
do Tempo e Estudos Clim{\'a}ticos (INPE.CPTEC) and Instituto
Nacional de Pesquisas Espaciais, Centro de Previs{\~a}o do Tempo
e Estudos Clim{\'a}ticos (INPE.CPTEC) and CIMA/UBA",
title = "Climatology of Low-Level Jet East of the Andes as derived from the
NCEP reanalyses",
booktitle = "Anais...",
year = "2002",
pages = "885--891",
organization = "Congresso Brasileiro de Meteorologia, 12.",
keywords = "METEOROLOGY, Climatology, Low-level jet, Andes mountains (South
America), METEOROLOGIA, Climatologia, Jato de baixo
n{\'{\i}}vel, Montanhas dos Andes (Am{\'e}rica do Sul).",
abstract = "A climatology of the Low Level Jet East of the Andes (LLJ)is
developed using the 1950-2000 circulation and moisture fields from
the NCEP reanalyses. Upper and low-level circulation fields were
determined for mean summer and wintertime, and for composites of
LLJ events during those seasons. The Bonner criterion 1 was
applied for circulation fields for sites en central Bolivia
(assumed as the core region), and in northern Paraguay (exit
region)to determine the spatial and temporal characteristics of
the LLJ. On the circulation characteristics, composites of
summertime LLJs shows the enhanced meridional moisture transport
coming from tropical South America. The upper level circulation
shows a wave train emanating from the West Pacific propagating
towards South America. The intensification of the LLJ obeys to the
establishment of an upper-level ridge over southern Brazil and a
trough over most of Argentina. Regarding the time variability, LLJ
seems to occur all year long, with the LLJ bringing tropical air
masses from the Amazon into southern Brazil-Northern Argentina
more frequent in summer, and the LLJ that brings subtropical air
from the Subtropical Atlantic High more frequent during winter.
The diurnal cycle shows that LLJs are more frequent and intense
between 06 and 12 (01 and 07 LST)for the warm season in the core
region of the jet, while at the exit region the maximum is
detected between 00 and 06 Z. during the cold season. This is
somewhat similar to the summertime LLJs in the US Great Plains. At
interannual time scales, even though there is a weak tendency for
stronger/more frequent LLJ episodes during El Ni¤o year 1998, we
cannot affirm with large degree of certainty that there is any
relationship between the occurrence of El Niņo events and the
number and/or intensity of LLJ episodes.",
conference-location = "Foz do Igua{\c{c}}u",
conference-year = "4-9 ago.",
copyholder = "SID/SCD",
language = "pt",
organisation = "SBMET",
targetfile = "Marengo_Climatology LLJ .pdf",
volume = "1",
urlaccessdate = "23 abr. 2024"
}