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Recommendations Emerging from PRA1 Discussion ( Diurnal and Mesoscale Variability)

Recommendations Emerging from PRA1 Discussion ( Diurnal and Mesoscale Variability). Precipitation in LPB comes mainly from large MCSs with intense convection, often related to transients. In the SACZ region, this is less so, and even less so in Amazonia

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Recommendations Emerging from PRA1 Discussion ( Diurnal and Mesoscale Variability)