ARCTIC Phytoplankton Chlorophyll Distribution- in the Eastern Canadian Arctic

Lancaster Sound, and Eastern Baffin Bay was studied dur-ing the period 16-27 August 1979, using continuous ship-based horizontal and vertical profiling and continuous aerial water colour measurements. These data are discussed in relation to physical data collected from the s ip, and to infrared temperature measurements made from the aircraft and the TIROS series satellites. While the satellite and airborne remote sensing techniques are capable only of viewing the near-surface layer. they provided a much more detailed and synoptic coverage of this large area than was possible using a vessel alone. Together the three types of data provide a reasonably detailed picture of phytoplankton distribution which compares well with other physical oceanographic data. On average the chlorophyll standing crop was moderate (69 mg.m-? in the top 35 m. n=24) and comparable to that reported for other open-water arctic regions, but the phytoplankton were not evenly distributed vertically or geographically. In Jones Sound and Lancaster Swnd where local ice melt reduced the surface water density, strong subsurface chlorophyll maxima (up to 18 mg.m-3 in a 1 m thick layer) were observed in association with the pycnocline. At the mouths of these sounds and along the eastern coast of Devon, Bylot, and Baffin islands the phytoplankton distribution was more vertically homogeneous and closely linked to the physical structure of the Baffin Current. Highest pigment concentrations were associated with eddies or meanders in the current. It is possible that these localized pigment concentrations are one manifestation of “biological hotspots ” which help feed the large populations of marine birds and mammals of the eastern Arctic. Key words: phytoplankton, chlorophyll, distribution, eastern Canadian Arctic, remote sensin