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The aim of this study was to characterize the small-scale variability (100s of meters to kilometers) of phytoplankton chlorophyll along cross-bay (lateral) flight tracks located in midand lower Chesapeake Bay over weekly, seasonal and interannual scales. Ana1ysc.s were made on aircraft ocean color data collected in 1990 and 1991 by NASA's Ocean Data Acquisitiun Systcm (ODAS). Lateral variability was highest durlng the spring bloom events of 1990 and was typically expressed as high westlow east gradients, particularly in the lower bay where up to 6-fold decreases in surface chlorophyll were found along a 15 km track. There was no spring bloom in 1991, which resulted in low lateral variability throughout the bay. These gradients appear to be associated with water masses that differ both physically and chemically along lateral transects. In the lower bay, phytoplankton patch size was within the resolution of future satellite sensors, which will provide even greater temporal coverage of the bay than that provided by aircraft.

Characterizing lateral variability of phytoplankton chlorophyll in Chesapeake Bay with aircraft ocean color data