Physical controls and interannual variability of the Labrador Sea spring phytoplankton bloom in distinct regions
Physical controls and interannual variability of the Labrador Sea spring phytoplankton bloom in distinct regions
We investigated the variability of the spring phytoplankton bloom in the Labrador Sea, dividing into distinct biogeographical zones, then analyzing the relationship between the bloom and physical forcings. The spring phytoplankton bloom in the north Labrador Sea varied in intensity by a factor of 4 and in timing of onset by 3 weeks over the 11-year record from SeaWiFS satellite ocean chlorophyll, 1998–2008. This north bloom (north of 60 °N and west of the Labrador shelves) is earliest and most intense, owing in part to the offshore-directed freshwater stratification from the West Greenland Current. On interannual timescales, significant correlations were found between the north bloom intensity and ocean processes, namely offshore advection, eddy activity and runoff from Greenland. In contrast, the central Labrador Sea is later and weaker, and only a correlation between the bloom timing and irradiance was found. As the subpolar gyre shifts in strength and shape, freshwater outflow from the Arctic and Greenland changes, we may expect further changes in the biological response as indicated by these relationships.
seawifs, spring bloom, physical controls, biophysical interactions, interannual variability, subpolar north atlantic, labrador sea
541-552
Frajka-Williams, Eleanor
da86044e-0f68-4cc9-8f60-7fdbc4dc19cb
Rhines, Peter B.
d65c16e0-07f7-4f88-a68d-609765d34dec
April 2010
Frajka-Williams, Eleanor
da86044e-0f68-4cc9-8f60-7fdbc4dc19cb
Rhines, Peter B.
d65c16e0-07f7-4f88-a68d-609765d34dec
Frajka-Williams, Eleanor and Rhines, Peter B.
(2010)
Physical controls and interannual variability of the Labrador Sea spring phytoplankton bloom in distinct regions.
Deep Sea Research Part I: Oceanographic Research Papers, 57 (4), .
(doi:10.1016/j.dsr.2010.01.003).
Abstract
We investigated the variability of the spring phytoplankton bloom in the Labrador Sea, dividing into distinct biogeographical zones, then analyzing the relationship between the bloom and physical forcings. The spring phytoplankton bloom in the north Labrador Sea varied in intensity by a factor of 4 and in timing of onset by 3 weeks over the 11-year record from SeaWiFS satellite ocean chlorophyll, 1998–2008. This north bloom (north of 60 °N and west of the Labrador shelves) is earliest and most intense, owing in part to the offshore-directed freshwater stratification from the West Greenland Current. On interannual timescales, significant correlations were found between the north bloom intensity and ocean processes, namely offshore advection, eddy activity and runoff from Greenland. In contrast, the central Labrador Sea is later and weaker, and only a correlation between the bloom timing and irradiance was found. As the subpolar gyre shifts in strength and shape, freshwater outflow from the Arctic and Greenland changes, we may expect further changes in the biological response as indicated by these relationships.
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FrajkaWilliams_Rhines_dsr2010.pdf
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e-pub ahead of print date: 21 January 2010
Published date: April 2010
Keywords:
seawifs, spring bloom, physical controls, biophysical interactions, interannual variability, subpolar north atlantic, labrador sea
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Local EPrints ID: 143703
URI: http://eprints.soton.ac.uk/id/eprint/143703
ISSN: 0967-0637
PURE UUID: ae89ff9d-67a1-473e-8ea5-b5c2bb9d7627
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Date deposited: 12 Apr 2010 16:01
Last modified: 14 Mar 2024 02:55
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Author:
Eleanor Frajka-Williams
Author:
Peter B. Rhines
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