Can Asian dust trigger phytoplankton blooms in the oligotrophic northern South China Sea?

Mathematics – Logic

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Atmospheric Composition And Structure: Pollution: Urban And Regional (0305, 0478, 4251, 4325), Biogeosciences: Remote Sensing, Geochemistry: Composition Of Aerosols And Dust Particles, Atmospheric Processes: Ocean/Atmosphere Interactions (0312, 4301, 4504), Oceanography: Biological And Chemical: Aerosols (0305, 4906)

Scientific paper

Satellite data estimate a high dust deposition flux (˜18 g m-2 a-1) into the northern South China Sea (SCS). However, observational evidence concerning any biological response to dust fertilization is sparse. In this study, we combined long-term aerosol and chlorophyll-a (Chl-a) measurements from satellite sensors (MODIS and SeaWiFS) with a 16-year record of dust events from surface PM10 observations to investigate dust transport, flux, and the changes in Chl-a concentration over the northern SCS. Our result revealed that readily identifiable strong dust events over this region, although relatively rare (6 cases since 1994) and accounting for only a small proportion of the total dust deposition (˜0.28 g m-2 a-1), do occur and could significantly enhance phytoplankton blooms. Following such events, the Chl-a concentration increased up to 4-fold, and generally doubled the springtime background value (0.15 mg m-3). We suggest these heavy dust events contain readily bioavailable iron and enhance the phytoplankton growth in the oligotrophic northern SCS.

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