Jc. Romano et F. Garabetian, PHOTOGRAPHIC RECORDS OF SEA-SURFACE MICROLAYERS AS A SURVEY OF POLLUTION DAILY RHYTHM IN COASTAL WATERS, Marine environmental research, 41(3), 1996, pp. 265-279
For one month photographic records of the sea surface were taken (ever
y five minutes) in a coastal area and used with records of wind speed
and direction to determine the frequency of formation and spatial exte
nt of slicks. The analysis of photographic records showed that slick s
izes and occurrence frequencies decrease as a direct function of the w
ind speed. When the weather is under the influence of local winds (hea
t flux exchanges between the sea and the continent), a periodic rhythm
occurs for a 24-h period: in the morning and late afternoon slicks ar
e generally large (coverage similar to 35%) and frequent (occurrence f
requency similar to 65%), but in the middle of the day, when the winds
increase to maximum velocity, slicks ave small (coverage similar to 1
2%) and rave (occurrence frequency <40%). During the night, a high sli
ck coverage (39%) can be deduced from wind conditions. The comparison
of the present data to the results of a previous experiment conducted
in another coastal area, and the fact that meteorological conditions w
hich have prevailed during this study were not particular, allow us to
extend our conclusions to the larger coastal zones. In situ sampling
in the surveyed area has shown higher concentrations of anionic deterg
ents and hydrocarbons in slicks as compared to the surrounding rough s
urface waters (Garabetian et al., 1993). Thus, this daily rhythm of sl
ick formation may have some important consequences for the dynamics of
pollutant dispersion.