Ship-based measurements in June 1994 provided information about ship-track
clouds and associated atmospheric environment observed from below cloud lev
els that provide a perspective different from satellite and aircraft measur
ements. Surface measurements of latent and sensible heat fluxes, sea surfac
e temperatures, and meteorological profiles with free and tethered balloons
provided necessary input conditions for models of ship track formation and
maintenance. Remote sensing measurements showed a coupling of ship plume d
ynamics and entrainment into overlaying clouds. Morphological and dynamic e
ffects were observed on clouds unique to the ship tracks. These morphologic
al changes included lower cloud bases early in the ship-track formation, ev
idence of raised cloud bases in more mature tracks, sometimes higher cloud
tops, thin cloud-free regions paralleling the tracks, and often stronger ra
dar returns. The ship-based lidar aerosol measurements revealed that ship p
lumes often interacted with the overlying clouds in an intermittent rather
than continuous manner. These observations imply that more must be learned
about ship-track dynamics before simple relations between cloud condensatio
n nuclei and cloud brightness can be developed.