INFLUENCES OF PHYSICAL OCEANOGRAPHIC PROCESSES ON CHLOROPHYLL DISTRIBUTIONS IN COASTAL AND ESTUARINE WATERS OF THE SOUTH ATLANTIC BIGHT

Coastal and estuarine waters of the South Atlantic Eight are highly pr oductive, with primary production of 600-700 gC/m2/y. While controls a nd fate of this production are conceptually well understood, the impor tance of meteorology and physical circulation processes on phytoplankt on has not received equivalent attention. Here, we describe the effect s of wind stress and tidal currents on temporal and spatial distributi ons of phytoplankton biomass represented as chlorophyll a (chl a). Moo red instruments were deployed and shipboard sampling was conducted in the North Edisto estuary (South Carolina) and adjacent inner shelf wat ers during four, two-week field studies in May and August 1993, and Ju ne and September 1994. Local wind regimes induced upwelling- and downw elling-favorable conditions which strengthened or reduced vertical den sity stratification in the coastal frontal zone, respectively, and shi fted the location of the front. Chi a in shelf waters was more or less homogenous independent of the wind regime, while chi a on the estuary delta was generally vertically stratified. Within the estuary, chi a concentrations were positively correlated with the alongshore componen t of wind stress; chi a was not correlated with the weaker cross-shelf component of wind stress. Highest chi a occurred during strong downwe lling-favorable events. The quick response time to wind forcing (6-12 hrs) implied a direct effect on chi a distributions and not a stimulat ion of growth processes. The source of the elevated chi a in response to wind forcing was apparently resuspension of settled and epibenthic algal cells. Tidal currents also influenced the vertical distribution and concentration of chi a. Time series sampling on the estuary delta showed that, with increasing velocity of ebb and flood tide currents, the relative contributions of pennate and centric diatoms with attache d detritus and sand grains also increased, indicating that tidal resus pension of settled and epibenthic microalgae also occurred. Vertical s tratification of chi a (highest concentrations near the bottom) began to degrade upon mixing by tidal currents with velocities as low as 10 cm/sec. Homogenization of 5-7 m water columns was fully achieved at ve locities of 20-30 cm/sec. The data document the direct and comparative ly immediate (timescales of minutes-hours) impact of tidal and wind en ergy on concentrations and distribution patterns of phytoplankton in c oastal and estuarine waters of the South Atlantic Eight.