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Optical proxy for particulate organic nitrogen from BGC-Argo floats.
Optics Express
|August 6, 2020
Summary
Scientists developed an optical proxy using backscattering to measure particulate organic nitrogen (PON) in the Western Tropical South Pacific. This method allows for improved monitoring of phytoplankton biomass and nitrogen dynamics in the region.
Area of Science:
- Oceanography
- Biogeochemistry
- Marine Optics
Background:
- Particulate organic nitrogen (PON) is a key nutrient influencing marine ecosystems.
- Accurate measurement of PON is crucial for understanding oceanic productivity and biogeochemical cycles.
- The Western Tropical South Pacific is an important region influenced by dinitrogen (N2) fixation.
Purpose of the Study:
- To develop and validate an optical proxy for particulate organic nitrogen (PON) concentration.
- To assess the relationship between the backscattering coefficient and PON in the Western Tropical South Pacific.
- To enable autonomous, large-scale monitoring of phytoplankton biomass dynamics using biogeochemical-Argo floats.
Main Methods:
- Utilized biogeochemical-Argo float measurements in the Western Tropical South Pacific.
- Measured the backscattering coefficient at 700 nm (bbp).
- Correlated bbp with particulate organic nitrogen (PON) concentrations determined by wet oxidation.
Main Results:
- Established a significant relationship (R2=0.87) between bbp and PON, particularly with wet oxidation measurements.
- Developed an optical proxy (PONopt) capable of estimating PON concentrations between 0.02 and 0.95 µM.
- Demonstrated PONopt as a reliable proxy for phytoplankton biomass in the study area.
- Observed significant increases in PONopt (0.16 to 0.80 µM) linked to N2 fixation during stratification.
Conclusions:
- The backscattering coefficient (bbp) serves as a viable optical proxy for PON concentration (PONopt).
- This optical proxy enables unprecedented autonomous monitoring of PON and phytoplankton biomass dynamics.
- The findings provide insights into new production linked to N2 fixation events in the Melanesian Archipelago.
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