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Estimating Oceanic Primary Production Using Vertical Irradiance and Chlorophyll Profiles from Ocean Gliders in the North Atlantic

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Figure

Figure 2. Scale factors calculated by optimization of modeled attenuation of irradiance against measured attenuation of irradiance (black ×) with the 10 day moving window (black line) and the standard deviation for each moving window (gray dashed line)
Figure 5. (a) Daily mean PP from Seaglider dives compared with in situ
Figure 6. Time series of PAR-corrected primary production profiles for SG566 for the entire deployment; the solid white line is the mixed layer depth (m), and the dashed white line is the euphotic depth (1% of surface irradiance levels).

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