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The planetary boundary layer (PBL) region of the atmosphere, is strongly influencied by the interaction with the surface. This paper studied the effect on PBL over the ocean using a coupled ocean-atmosphere-wave-sediment transport numerical model (COAWST). It was done two experiments, one with COAWST and another with atmospheric model WRF.

EFEITO DO ACOPLAMENTO DOS MODELOS NUMÉRICOS ROMS-WRF NA CAMADA LIMITE PLANETÁRIA – UM ESTUDO DE CASO SOBRE A CONFLUÊNCIA BRASIL-MALVIAS