2013
DOI: 10.5194/adgeo-35-79-2013
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Comparison results for the CFSv2 hindcasts and statistical downscaling over the northeast of Brazil

Abstract: Abstract. An Artificial Neural Networks (ANNs) approach was used to reproduce the precipitation anomalies for the rainy seasons over the south and north parts of the Northeast of Brazil (NEB) during 1982–2009 period. The seasonal hindcasts of precipitation anomalies from Climate Forecast System v2 (CFSv2) model and the observed dominant modes of anomalous Sea Surface Temperature over the South and North Atlantic Ocean were used as explanatory variables separately. The reduction of dispersion between the explan… Show more

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Cited by 9 publications
(11 citation statements)
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“…Also, the differences between the normalized time series of the observed daily precipitation and the CMIP5 simulations during FMA season are shown. To explain such differences is calculated the anomalies of SST and precipitation over the Atlantic Ocean using as observations the ERSST version3b (Smith et al, 2008) FIGURE 1 | Location of the study region: North of the NEB delimited by the red box between 2 and 7 • S; 40 and 45 • W. The location is similar as in Silva and Mendes (2013). Adapted from http://mapas.ibge.gov.br.…”
Section: Methodsmentioning
confidence: 99%
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“…Also, the differences between the normalized time series of the observed daily precipitation and the CMIP5 simulations during FMA season are shown. To explain such differences is calculated the anomalies of SST and precipitation over the Atlantic Ocean using as observations the ERSST version3b (Smith et al, 2008) FIGURE 1 | Location of the study region: North of the NEB delimited by the red box between 2 and 7 • S; 40 and 45 • W. The location is similar as in Silva and Mendes (2013). Adapted from http://mapas.ibge.gov.br.…”
Section: Methodsmentioning
confidence: 99%
“…As in Silva and Mendes (2013) the Multilayer Perceptron architecture is used that is more adequate network for meteorological applications because the weather and the climate can repeat along the chronological time but never exactly in the same way (e.g., Cardoso and da Silva Dias, 2004 represent the topology of the ANN used in the present study for the present and future climate analyses, respectively. For both simulations the Multilayer Perceptron topology is interconnected in a feed-forward method.…”
Section: Methodsmentioning
confidence: 99%
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“…The increase of extreme events in a short period of time became in the society more vulnerable at weather and climate extremes variability, resulting in great socioeconomic losses [1]. These extremes are related to several environmental factors that favor the increase on their frequency and intensity: 1) ocean-atmospheric variables relationships, such as: air temperature [2], precipitation [3], wind speed [4] and sea surface temperature (SST) [5]; 2) regional micro-climate changes due to rapid urbanization of the cities without proper urban planning [6]; and 3) orographic effects [7]. These factors when combined at atmospheric circulation or meteorological systems in several spatiotemporal scales [8] can favor the extremes occurrence; the aim of this paper is to diagnose the precipitation extremes.…”
Section: Introductionmentioning
confidence: 99%
“…In relation to the application of non-destructive techniques to characterize the ground conditions of any site, Tokeshi et al (2013) assessed the ground compaction and general geotechnical site characterization based on the application of non-invasive Multichannel Analysis of Surface Waves (MASW) and Multichannel Simulation with One Receiver (MSOR) techniques.…”
mentioning
confidence: 99%