2020
DOI: 10.1590/0102-77863550071
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Desenvolvimento de Atividades Convectivas Sobre a Região Nordeste do Brasil, Organizada Pela Extremidade Frontal

Abstract: Resumo Nas extremidades de zonas frontais que atingem o Nordeste brasileiro (NEB), em alguns eventos, desenvolve-se convecção, e em outras frentes isso não ocorre. Os eventos em que ocorre convecção profunda sobre o NEB, estão associados a eventos de precipitação intensa e possíveis transtornos associados. Por isso, o objetivo geral é analisar as diferenças dos processos dinâmicos e termodinâmicos nestes eventos e obter os padrões de circulação. Foram utilizados dados de reanálise do modelo global do NCEP/NCAR… Show more

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“…Ceará has seven mesoregions (Figure 10), due to the dismemberment of the municipalities bordering the capital, which formed the Metropolitana de Fortaleza mesoregion (Figure 10b). Throughout the state, the wettest period is the JFMAMJ semester, influenced by systems such as upper tropospheric cyclonic vortices (UTCV), which peak between January and February [44], ITCZ between February and April [45], remnants of easterly wave disturbances (EWD) in May and June [46], in addition to the interaction between larger-scale phenomena, such as frontal systems that induce the formation of mesoscale convective complexes [47,48]. However, as in the entire northern sector of the NEB, there is great interannual variability and poor spatial-temporal distribution of rainfall in the growing season, reflecting in years with higher and lower production.…”
Section: Results By State-cearámentioning
confidence: 99%
“…Ceará has seven mesoregions (Figure 10), due to the dismemberment of the municipalities bordering the capital, which formed the Metropolitana de Fortaleza mesoregion (Figure 10b). Throughout the state, the wettest period is the JFMAMJ semester, influenced by systems such as upper tropospheric cyclonic vortices (UTCV), which peak between January and February [44], ITCZ between February and April [45], remnants of easterly wave disturbances (EWD) in May and June [46], in addition to the interaction between larger-scale phenomena, such as frontal systems that induce the formation of mesoscale convective complexes [47,48]. However, as in the entire northern sector of the NEB, there is great interannual variability and poor spatial-temporal distribution of rainfall in the growing season, reflecting in years with higher and lower production.…”
Section: Results By State-cearámentioning
confidence: 99%