PHOTOGRAPHIC RECORDS OF SEA-SURFACE MICROLAYERS AS A SURVEY OF POLLUTION DAILY RHYTHM IN COASTAL WATERS

Citation
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
Citations number
39
Categorie Soggetti
Marine & Freshwater Biology","Environmental Sciences",Toxicology
ISSN journal
01411136
Volume
41
Issue
3
Year of publication
1996
Pages
265 - 279
Database
ISI
SICI code
0141-1136(1996)41:3<265:PROSMA>2.0.ZU;2-7
Abstract
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.