BIOOPTICAL AND PHYSICAL VARIABILITY IN THE SUB-ARCTIC NORTH-ATLANTIC OCEAN DURING THE SPRING OF 1989

A unique set of physical, bio-optical, and meteorological observations were made from a mooring located in the open ocean south of Iceland ( 59 degrees 29.5'N, 20 degrees 49.8'W) from April 13 to June 12, 1989. The present measurements are apparently the first to resolve the rapid transition to springtime physical and biological conditions at-such a high latitude site. Our data were collected with bio-optical and phys ical moored systems every few minutes. The abrupt onset of springtime stratification was observed with the mixed layer shoaling from similar to 550 m to similar to 50 m in similar to 5 days. During this period a major phytoplankton bloom occurred with a tenfold increase in near-s urface chlorophyll concentration in less than 3 weeks. Our statistical analysis indicates that the velocity shear in the upper layer is driv en primarily by local wind stress. Mesoscale variability is also appar ent from these and concurrent airborne oceanographic lidar observation s. Our complementary modeling results suggest that the near-surface la yer may be reasonably well described by a one-dimensional model and th at the spring bloom was initiated during incipient near-surface restra tification.