Abstract

Abstract. A new method of retrieving the parameters of a power-law particle size distribution (PSD) from ocean color remote sensing data was used to assess the global distribution and dynamics of phytoplankton functional types (PFT's). The method retrieves the power-law slope, ξ, and the abundance at a reference diameter, N0, based upon the shape and magnitude of the particulate backscattering coefficient spectrum. Relating the PSD to PFT's on global scales assumes that the open ocean particulate assemblage is biogenic. The retrieved PSD's can be integrated to define three size-based PFT's by the percent volume concentration contribution of three phytoplankton size classes – picoplankton (0.5–2 μm in equivalent spherical diameter), nanoplankton (2–20 μm) and microplankton (20–50 μm). Validation with in-situ HPLC diagnostic pigments resulted in better match-ups for the pico- and micro-phytoplankton size classes as compared to nanoplankton. Global decadal averages derived from SeaWiFS monthly data reveal PFT and particle abundance spatial patterns that are consistent with current understanding. Oligotrophic gyres are characterized by lower particle abundance and higher contribution by picoplankton-sized particles than transitional or eutrophic regions. Seasonal succession patterns for size-based PFT's reveal good correspondence between increasing chlorophyll concentration and percent contribution by microplankton, as well as increasing particle abundance. Long-term trends in particle abundances are generally well correlated with the MEI index indicating increased oligotrophy (i.e. lower particle abundance and increased contribution of picoplankton-sized particles) during the warm phase of an El Niño event. This work demonstrates the utility and future potential of assessing phytoplankton functional types using remote characterization of the particle size distribution.

Highlights

  • The World Ocean profoundly influences Earth’s habitability and plays a key role in the formation and regulation of climate via several key physical and biological processes and the ensuing feedbacks (IPCC, 2007)

  • The SeaWiFS nanoplantkon retrievals showed a cluster of results near 50%, which was not seen in the in-situ observations

  • We explored the global and regional effects of El Nino – Southern Oscillation (ENSO) on SST, chl, the particle size distribution (PSD)-derived phytoplankton functional types (PFT’s) and other relevant variables

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Summary

Introduction

The World Ocean profoundly influences Earth’s habitability and plays a key role in the formation and regulation of climate via several key physical and biological processes and the ensuing feedbacks (IPCC, 2007). Oxygenic photosynthetic activity by phytoplankton was the single most important factor that led to the current oxygen replete atmosphere The biological pump, powered by phytoplankton photosynthesis, is one of the ways that ocean biology influences atmospheric CO2 concentration, by altering the rain of organic particles to depth. Oceanic ecosystems are composed of microbes with different functions and biogeochemical roles. Small pico-phytoplankton species dominate the oligotrophic regions of the sea because of their efficiency in utilizing remineralized nutrients, whereas large phytoplankton groups such as diatoms are found in nutrient replete waters and their presence increases the efficiency of the biological pump Understanding the spatial and temporal distribution and variability of different phytoplankton species according to their

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