Understanding the droplet cloud and spray dynamics is important on the study of the ocean surface and marine boundary layer. Several of the relevant phenomena depend highly on the characteristics of the spray produced by waves. Nonetheless, the role that the wave energy and the type of wave breaking plays in the resulting distribution and dynamics of droplets is yet to be understood. The aim of this work was to generate violent plunging breakers in the laboratory, quantify the produced droplets, obtaining their sizes and dynamics and to analyze the effect of the different wind speeds on the droplet production. It was found that the mean radius increases with the wave energy and the shape of the initial distribution of droplet sizes does not change with the presence of wind. Also, indications of turbulence affecting the droplet dynamics at wind speeds of 5m/s were found. The amount of large droplets (radius > 1mm) found in this work was larger than expected from the literature. An improved estimation of the initial distribution of large droplets can largely affect the evolution of the Sea Spray Generation Function, and therefore the estimation of energy and mass transport in the marine boundary layer.