4.7 Article

Southern Ocean Phytoplankton Blooms Observed by Biogeochemical Floats

Journal

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
Volume 124, Issue 11, Pages 7328-7343

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2019JC015355

Keywords

Southern Ocean; phytoplankton bloom; Argo; SOCCOM; SOCLIM

Categories

Funding

  1. NASA as part of the SWOT Science Team [NNX14AP49G]
  2. NSF [PLR-1425989, OCE-1658001, OCE-1553593, DGE-1650112]
  3. National Science Foundation, Division of Polar Programs [NSF PLR-1425989]
  4. NASA [NNX14AP49G]
  5. Foundation BNP Paribas
  6. Massachusetts Water Resource Authority
  7. International Argo Program
  8. NOAA programs
  9. NSF XSEDE resource Grant [OCE130007]
  10. CNES

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The spring bloom in the Southern Ocean is the rapid-growth phase of the seasonal cycle in phytoplankton. Many previous studies have characterized the spring bloom using chlorophyll estimates from satellite ocean color observations. Assumptions regarding the chlorophyll-to-carbon ratio within phytoplankton and vertical structure of biogeochemical variables lead to uncertainty in satellite-based estimates of phytoplankton carbon biomass. Here, we revisit the characterizations of the bloom using optical backscatter from biogeochemical floats deployed by the Southern Ocean Carbon and Climate Observations and Modeling and Southern Ocean and Climate Field Studies with Innovative Tools projects. In particular, by providing a three-dimensional view of the seasonal cycle, we are able to identify basin-wide bloom characteristics corresponding to physical features; biomass is low in Ekman downwelling regions north of the Antarctic Circumpolar Current region and high within and south of the Antarctic Circumpolar Current.

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