2014
DOI: 10.5902/2179460x12579
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Estudo Preliminar Da Aplicação Da Teoria De Dutos Atmosféricos Às Linhas De Instabilidade Amazônicas

Abstract: Este trabalho apresenta uma análise de perfis do vento e de temperatura potencial e temperatura potencial equivalente em sítios localizados pró

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“…Although the rainfall in different parts of the North and South‐east Coast group has similar characteristics in terms of events and their properties, the mechanisms of precipitation formation are different among the areas of this group. For instance, the precipitation in the northern area of this group, corresponding to the Amazon rainforest, is mainly caused by the influence of the Intertropical Convergence Zone (ITCZ) (Amanajás & Braga, 2012; Santos et al, 2015), squall lines (Alcântara, 2011; Fisch et al, 1996), and the radiative heating of the surface, which can generate convective cells typical of tropical regions (mesoscale convective complex, MCC) (Nobre et al, 2009; Strong et al, 2005). Within this area, the differences between northern and southern Amazonia are consistent with the results of Marengo (2004) and Santos et al (2015), who attributed them to different rain‐triggering systems.…”
Section: Resultsmentioning
confidence: 99%
“…Although the rainfall in different parts of the North and South‐east Coast group has similar characteristics in terms of events and their properties, the mechanisms of precipitation formation are different among the areas of this group. For instance, the precipitation in the northern area of this group, corresponding to the Amazon rainforest, is mainly caused by the influence of the Intertropical Convergence Zone (ITCZ) (Amanajás & Braga, 2012; Santos et al, 2015), squall lines (Alcântara, 2011; Fisch et al, 1996), and the radiative heating of the surface, which can generate convective cells typical of tropical regions (mesoscale convective complex, MCC) (Nobre et al, 2009; Strong et al, 2005). Within this area, the differences between northern and southern Amazonia are consistent with the results of Marengo (2004) and Santos et al (2015), who attributed them to different rain‐triggering systems.…”
Section: Resultsmentioning
confidence: 99%