2016
DOI: 10.1590/0102-778620150017
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Início e Fim da Estação Chuvosa no Estado de Minas Gerais: Comparação de Duas Metodologias Diferentes

Abstract: Resumo O Início e Fim da Estação Chuvosa (IEC e FEC, respectivamente) são encontrados em Minas Gerais (MG) para 1998-2012 através de duas metodologias: uma que utiliza dados diários de precipitação e outra que utiliza dados diários de Radiação de Onda Longa antissimétrico equatorialmente (ROLant). O IEC (FEC) é indicado pela mudança de sinal positivo-negativo (negativo-positivo) das médias espaciais do ROLant, como em Garcia e Kayano (2009; 2013), e, pelo método de Liebmann et al. (2007), determina-se pelo mín… Show more

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Cited by 6 publications
(5 citation statements)
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“…In this analysis, we used the daily precipitation from the Climate Hazards Group InfraRed Precipitation with Station data (CHIRPS) [80], which has the advantage of incorporating 0.05 • resolution satellite imagery with in situ station data. The determination of the onset/demise dates and the length of the rainy season in the Amazon region and South America have already been investigated by different methods [7,77,78,[81][82][83][84][85]. However, the method used in our study was sufficient for our purpose.…”
Section: Identification Of the Onset And Demise Of The Rainy Seasonmentioning
confidence: 99%
“…In this analysis, we used the daily precipitation from the Climate Hazards Group InfraRed Precipitation with Station data (CHIRPS) [80], which has the advantage of incorporating 0.05 • resolution satellite imagery with in situ station data. The determination of the onset/demise dates and the length of the rainy season in the Amazon region and South America have already been investigated by different methods [7,77,78,[81][82][83][84][85]. However, the method used in our study was sufficient for our purpose.…”
Section: Identification Of the Onset And Demise Of The Rainy Seasonmentioning
confidence: 99%
“…O ciclo anual climatológico de precipitação em MG é bem definido, com inverno seco (Figuras 2a-2c) e verão chuvoso (Figuras 2g-2i), consistente à climatologia de precipitação do estado mostrada por Silva e Reboita (2014) e Reboita et al (2015),com períodos de transição na primavera e no outono (Figuras 2d-2l). Esses resultados são característicos do Sistema de Monção da América do Sul (SMAS) (RAO et al, 1996;ZHOU;LAU, 1998;GARCIA, 2016;GARCIA et al, 2016a;2016b).O ciclo sazonal da precipitação do SMAS tem início na Amazônia equatorial, propaga-se rapidamente para leste e sudeste no final de setembro e início de outubro, gerando uma estação úmida com chuvas abundantes na Bacia Amazônica. Na fase madura do SMAS (final de novembro até final de fevereiro), essa atividade convectiva da região amazônica estende a precipitação sobre o sudeste do Brasil e o oceano Atlântico adjacente, caracterizando uma banda de nebulosidade, a Zona de Convergência do Atlântico Sul (KODAMA, 1993).…”
Section: 1análise Climatológicaunclassified
“…The presence of total coliforms and E. coli in the water supply and distribution system persisted throughout the study months, and from July 2017 total coliform contamination was present in all samples analyzed. For E. coli, the highest frequencies of contamination were observed during the rainy season, between November and March (Santos and Garcia, 2016), especially in November/2017, January and February 2018, where percentage of contamination were 55.5%, 100.0% and 88.9%, respectively. The result is in agreement with the fact that there is a consensus that the worsening tendency of water quality in rainy periods is a consequence of the drag of organic matter and various particles, which protect the microorganisms from contact with chemical disinfectants, which favors its viability (Gleason and Fagliano, 2017).…”
Section: Resultsmentioning
confidence: 96%