Possible role of electric forces in bromine activation during polar boundary layer ozone depletion and aerosol formation events

According to the author's estimates, high wind can generate sufficient conditions for overcoming the Rayleigh limit and thus can initiate “spraying” of charged aerosol nanoparticles. These charged aerosol nanoparticles can provoke formation of free radicals, turning the ODE on. One can also envision a possible emission of halogen ion as a result of the “electrospray” process analogous to that of electrospray ionization mass-spectrometry.