@Article{MarengoRustPenaReno:2010:Pa2:Hi,
author = "Marengo, Jos{\'e} Antonio and Rusticucci, Matilde and Penalba,
Olga and Renom, Madeleine",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE/CPTEC)} and
Departamento de Ciencias de la Atm{\'o}sfera y los Oc{\'e}anos
FCEN Universidad de Buenos Aires, Buenos Aires, Argentina and
Departamento de Ciencias de la Atm{\'o}sfera y los Oc{\'e}anos
FCEN Universidad de Buenos Aires, Buenos Aires, Argentina and
4Unidad Ciencias de la Atm{\'o}sfera, FCIEN, Universidad de la
Republica, Montevideo, Uruguay",
title = "An intercomparison of observed and simulated extreme rainfall and
temperature events during the last half of the twentieth century:
part 2: historical trends",
journal = "Climatic Change",
year = "2010",
volume = "98",
number = "3-4 Special Issue",
pages = "509--529",
month = "feb",
keywords = "atlantic convergence zone, sea surface temperature, South America,
climate change, precipitation events, Argentina, variability,
circulation, Brazil.",
abstract = "Projections of changes in climate extremes are critical to
assessing the potential impacts of climate change on human and
natural systems. Therefore, especial care should be put on the
validation of those extremes derived for present climate in both
spatial and temporal variability. We analyze historical
simulations of three such indicators as derived from seven GCMs
contributing to the Fourth Assessment Report of the
Intergovernmental Panel on Climate Change (IPCC-AR4) for the XX
century. Our focus is on the consensus in the geographical and
temporal variability of temperature and rainfall extreme trends
between observations and the GCMs, in terms of direction and
significance of the changes at the scale of South America south of
10 oS. The climate extremes described by the 3 indices include
warm nights, heavy rainfall amounts and dry spells. The observed
historical trends in extremes generally agree with previous
observational studies that used other indicators of extremes, and
the favorable comparison in the warm nights and extreme rainfall
in some regions provides a basic sense of reliability for the GCM
simulations. For any specific temperature index, minor differences
appear in the spatial distribution of the changes across models in
some regions, while substantial differences appear in regions in
interior tropical and subtropical South America. The differences
are in the relative magnitude of the trends. Consensus and
significance are less strong when regional patterns are
considered, with the exception of the La Plata Basin, where
observed and simulated trends in warm nights and extreme rainfall
are evident. This analysis provides a first overview of simulated
trends in extremes for present climates, and further work is
focused on projected changes in climate extremes from the IPCC-AR4
models.",
doi = "10.1007/s10584-009-9743-7",
url = "http://dx.doi.org/10.1007/s10584-009-9743-7",
issn = "0165-0009",
language = "en",
targetfile = "Marengo Intercomparison.pdf",
urlaccessdate = "16 jun. 2024"
}