SeaWiFS satellite ocean color data from the Southern Ocean

• Published in: Geophysical Research Letters
• Main Authors: Moore, J. Keith, Abbott, Mark R, Richman, James G, Smith, Walker O, Cowles, Timothy J, Coale, Kenneth H, Gardner, Wilford D, Barber, Richard T
• Format: Article in Journal/Newspaper
• Language: English
• Published: eScholarship, University of California 1999
• Subjects: Physical Sciences and Mathematics; phytoplankton; Antarctic; Southern Ocean; The Antarctic; Pacific; Antarc*; Ice Sheet
• Online Access: http://www.escholarship.org/uc/item/9rt8q4qt

SeaWiFS estimates of surface chlorophyll concentrations are reported for the region of the U.S. JGOFS study in the Southern Ocean (∼ 170°W, 60°S). Elevated chlorophyll was observed at the Southern Ocean fronts, near the edge of the seasonal ice sheet, and above the Pacific-Antarctic Ridge. The elevated chlorophyll levels associated with the Pacific-Antarctic Ridge are surprising since even the crest of the ridge is at depths > 2000 m. This elevated phytoplankton biomass is likely the result of mesoscale physical-biological interactions where the Antarctic Circumpolar Current (ACC) encounters the ridge. Four cruises surveyed this region between October 1997 and March 1998, as part of the U.S. JGOFS. Satellite-derived chlorophyll concentrations were compared with in situ extracted chlorophyll measurements from these cruises. There was good agreement (r² of 0.72, from a linear regression of shipboard vs. satellite chlorophyll), although SeaWiFS underestimated chlorophyll concentrations relative to the ship data.