@Article{MarengoValvObre:2013:ObPrCh,
author = "Marengo, Jos{\'e} Antonio and Valverde, Maria C. and Obregon,
Guillermo O.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Federal
University of ABC (UFABC)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)}",
title = "Observed and projected changes in rainfall extremes in the
metropolitan area of S{\~a}o Paulo",
journal = "Climate Research",
year = "2013",
volume = "57",
number = "1",
pages = "61--72",
keywords = "climate assessment, dynamical downscaling, emissions scenarios,
extreme precipitation events, heavy precipitation, metropolitan
area, natural climate variabilities, total precipitation, climate
change, climate models, floods, uncertainty analysis, rain,
climate modeling, climate variation, downscaling, extreme event,
flash flood, flooding, future prospect, landslide, metropolitan
area, precipitation, prediction, trend analysis, uncertainty
analysis, urbanization, weather forecasting.",
abstract = "Changes in rainfall extremes and flooding are becoming more
frequent in many countries, particularly in large cities where
people and assets are concentrated. In the Metropolitan Area of
the city of S{\~a}o Paulo (MASP) region, heavy or extreme
precipitation events have important effects on society. Flash
floods and landslides, associated with intense, but often brief,
rainfall events, may be the most destructive of extreme events.
Observations since the mid-1930s in the MASP region have shown
significant increases in total and heavy rainfall and decreases in
light rain. This was probably due to natural climate variability,
but with some signals of the urbanization effect, especially
during the last 40 yr. Here projections of future changes in
rainfall extremes in the MASP region were derived from the
Eta-CPTEC 40 km regional model nested in the HadCM3 global model,
with 4 available realizations of the global model for the A1B
emissions scenario to the end of the 21st century. Trends were
assessed for significance using the nonparametric Mann-Kendall
test. Projections, based on percentiles and on the number of days
with rainfall above a certain limit, suggested: (a) an increase in
total precipitation, (b) an increase in heavy precipitation and in
the contribution to total precipitation from more intense rainfall
events, and (c) the possibility of longer dry periods separating
days with intense rain in the MASP region. The trends were
stronger and more significant in the second half of the 21st
century. We are aware that dynamical downscaling may not provide
information at the weather station level and that climate modeling
does not resolve all uncertainties. However, we believe that this
exercise enables climate assessments that, in time, can be used
for general public information.",
doi = "10.3354/cr01160",
url = "http://dx.doi.org/10.3354/cr01160",
issn = "0936-577X",
label = "scopus 2013-11",
language = "en",
targetfile = "c057p061.pdf",
urlaccessdate = "21 maio 2024"
}