Research news on maritime cloud

A maritime cloud is a low-level cloud formation that develops over oceanic regions, typically within the marine boundary layer, and is strongly modulated by sea surface temperature, atmospheric stability, and aerosol availability. These clouds, often stratocumulus or cumulus, form in a moist but relatively clean environment where cloud condensation nuclei concentrations are generally lower than over continents, affecting droplet number, size distributions, and albedo. Maritime clouds exert a significant influence on the surface energy budget and large-scale circulation by modulating shortwave reflection and longwave emission, and they play a central role in cloud–aerosol interactions, cloud feedbacks, and precipitation efficiency in marine meteorology and climate system studies.