The aerosol concentration over the ocean depends mostly on wave breaking and the wind speed. However, the wind speed is somehow included in the wind input source term which on the other hand influences the breaking source term. Having knowledge of breaking intensity and breaking probability from the breaking source term there could be maybe somebody that did this work to derive a formula for aerosol concentration. Of course it is finally aerosol concentration profile, which will somehow follow the Rouse profile. However in order to define some concentration profile we need the reference concentration (Ca) at a reference height (a). What the reference height "a" will be is also a matter of question, maybe Hs? Any literature reference would be nice ...
Thanks in advance