Processos de Desestabilização Atmosférica e Convecção Profunda no Semiárido Brasileiro
DOI:
https://doi.org/10.5902/2179460X11639Abstract
O desenvolvimento deste trabalho tem como objetivo identificar mecanismos importantes no processo de desestabilização atmosférica e evolução da atividade convectiva. O grau de instabilidade atmosférica aliado ao teor e transporte zonal de umidade na baixa troposfera foi identificado através de uma análise fatorial em componentes principais como os principais fatores na ocorrência da convecção profunda e chuva intensa observadas em janeiro de 2004 no semiárido brasileiro.Downloads
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