@Article{HaylockPAAABBBBCCGGKMMMNQRRSTV:2006:TrToEx,
author = "Haylock, M. R. and Peterson, T. C. and Alves, Lincoln Muniz and
Ambrizzi, Tercio and Anuncia{\c{c}}{\~a}o, Y. M. T. and Baez, J.
and Barros, V. R. and Berlato, M. A. and Bidegain, M. and Coronel,
G. and Corradi, V. and Garcia, V. J. and Grimm, A. M. and Karoly,
D. and Marengo, Jose Antonio and Marino, M. B. and Muncunil, D. F
and Nechet, D. and Quintana, J. and Rebello, E. and Rusticucci, M.
and Santos, J. L. and Trebejo, I. and Vincent, L.",
affiliation = "University of East Anglia, Climatic Research Unit and {National
Climatic Data Center} and Instituto Nacional de Pesquisas
Espaciais, Centro de Previs{\~a}o de Tempo e Estudos
Clim{\'a}ticos (INPE.CPTEC) and {Universidade de S{\~a}o Paulo
(USP)} and {Instituto Nacional de Meteorologia (INMET)} and
{Dirreccion de Meteorologio e Hidrologio} and Departamento de
Ciencias de la Atmosfera y los Oceanos, Universidad de Buenos
Aires and {Universidade Federal do Rio Grande do Sul (UFRGS)} and
Faculty of Science, Universidad de la Republica and {Universidad
Nacional de Asuncion} and {Direccion Nacional de Meterologia} and
{Universidad Nacional Agraria la Molina} and {Universidade Federal
do Paran{\'a} (UFPR)} and {University of Oklahoma} and Instituto
Nacional de Pesquisas Espaciais, Centro de Previs{\~a}o do Tempo
e Estudos Clim{\'a}ticos (INPE.CPTEC) and Banco Nacional de
Datos, Servicio Meteorologico Nacional and {Funda{\c{c}}{\~a}o
Cearense de Meteorologia e Recursos H{\'{\i}}dricos (FUNCEME)}
and {Universidade Federal do Par{\'a} (UFPA)} and {Direcci{\'o}n
Meteorol{\'o}gica de Chile} and {Instituto Nacional de
Meteorologia (INMET)} and {Departamento de Ciencias de la
Atmosfera y los Oceanos} and Faculty of Marine Sciences, Escuela
Superior Politecnica del Litoral and {Servicio Nacional de
Meteorologia e Hidrologia} and {Meteorological Service of
Canada}",
title = "Trends in total and extreme South American rainfall 1960-2000 and
links with sea surface temperature",
journal = "Journal of Climate",
year = "2006",
volume = "19",
number = "8",
pages = "1490--1512",
month = "April",
keywords = "METEOROLOGY, South America, Rainfall, Sea surface termperature,
METEOROLOGIA, Am{\'e}rica do Sul, Pluviosidade, Termperatura de
superf{\'{\i}}cie do mar.",
abstract = "A weeklong workshop in Brazil in August 2004 provided the
opportunity for twenty-eight scientists from southern South
America to examine daily rainfall observations to determine
changes in both total and extreme rainfall. Twelve annual indices
of daily rainfall were calculated over the period 1960 to 2000,
examining changes to both the entire distribution as well as the
extremes. Maps of trends in the twelve rainfall indices showed
large regions of coherent change, with many stations showing
statistically significant changes in some of the indices. The
pattern of trends for the extremes was generally the same as that
for total annual rainfall, with a change to wetter conditions in
Ecuador and northern Peru and the region of southern Brazil,
Paraguay, Uruguay and northern and central Argentina. A decrease
was observed in southern Peru and southern Chile, with the latter
showing significant decreases in many indices. A canonical
correlation analysis between each of the indices and sea surface
temperatures (SST) revealed two large-scale patterns that have
contributed to the observed trends in the rainfall indices. A
coupled pattern with ENSO-like SST loadings and rainfall loadings
closely resembling the pattern of the observed trend reveals that
the change to a generally more negative SOI has had an important
effect on regional rainfall trends. A significant decrease in many
of the rainfall indices at several stations in southern Chile and
Argentina can be explained by a canonical pattern reflecting a
weakening of the continental trough leading to a southward shift
in storm tracks. This latter signal is a change that has been seen
at similar latitudes in other parts of the Southern Hemisphere. A
similar analysis was carried out for eastern Brazil using gridded
indices calculated from 354 stations from the Global Historical
Climatology Network (GHCN) database. The observed trend toward
wetter conditions in the southwest and drier conditions in the
northeast could again be explained by changes in ENSO.",
copyholder = "SID/SCD",
issn = "0894-8755",
language = "en",
targetfile = "zs4.pdf",
urlaccessdate = "03 maio 2024"
}