Motivated by the meteorological question whether a turbulent velocity field accelerates rain droplets merging and favors rain, we prove that for a system of locally interacting diffusions carrying discrete masses, subject to an environmental noise and undergoing mass coagulation, its empirical measures corresponding to different masses converge to a system of Stochastic Partial Differential Equations (SPDEs) with enhanced diffusion coefficient and Smoluchowskitype nonlinearity. Existence, uniqueness and regularity of the SPDEs are proved, which can be of independent interest.