CIMA   09099
CENTRO DE INVESTIGACIONES DEL MAR Y LA ATMOSFERA
Unidad Ejecutora - UE
artículos
Título:
South America Overview in State of the Climate in 2007
Autor/es:
PATRICIO LOPEZ; RUSTICUCCI MATILDE
Revista:
BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY
Editorial:
American Meteorological Society
Referencias:
Año: 2008 vol. 89 p. 124 - 131
ISSN:
0003-0007
Resumen:
The data used in this section were acquired from
300 meteorological stations by the National Meteorological
and Hydrological Services of Argentina,rological
and Hydrological Services of Argentina,
Bolivia, Brazil, Chile, Colombia, Ecuador, Guyana,
Paraguay, Perú, Surinam, Uruguay, and Venezuela.
The data were compiled by CIIFEN.
In general terms, climate conditions over South
America during 2007 were drier than normal in the
southern and eastern parts of the continent, very dry
over the west, and near normal to wetter than normal
in the region north of the equator and parts of the
Amazon basin (Fig. 6.21). With regard to temperatures,
an unusually cold winter was reported over
the southern portion of the continent, while warmerthan-
normal conditions prevailed in the Amazonian
region. This marked meridional contrast in temperature,
between the anomalously warm conditions in
the tropics and the lower-than-normal temperature
over the southern half of the continent, was observed
for 2007 as a whole in terms of mean, maximum, and
minimum temperatures (Fig. 6.22).
The weak El Niño conditions in January quickly
rological
and Hydrological Services of Argentina,
Bolivia, Brazil, Chile, Colombia, Ecuador, Guyana,
Paraguay, Perú, Surinam, Uruguay, and Venezuela.
The data were compiled by CIIFEN.
In general terms, climate conditions over South
America during 2007 were drier than normal in the
southern and eastern parts of the continent, very dry
over the west, and near normal to wetter than normal
in the region north of the equator and parts of the
Amazon basin (Fig. 6.21). With regard to temperatures,
an unusually cold winter was reported over
the southern portion of the continent, while warmerthan-
normal conditions prevailed in the Amazonian
region. This marked meridional contrast in temperature,
between the anomalously warm conditions in
the tropics and the lower-than-normal temperature
over the southern half of the continent, was observed
for 2007 as a whole in terms of mean, maximum, and
minimum temperatures (Fig. 6.22).