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The advent of remote sensing, the development of new optical instrumentation, and the associated advances in hydrological optics have transformed oceanography: it is now feasible to describe ocean‐scale biogeochemical dynamics from satellite observations, verified and complemented by measurements from optical sensors on profilers, moorings, and drifters. Only near‐surface observations are common to both remote sensing and in situ observation, so it is critical to understand processes in the upper euphotic zone. Unfortunately, the biological principles that must be used to interpret optical variability near the sea surface are weaker than we would like, because relatively few experiments and analyses have examined bio‐optical relationships under high irradiance characteristic of the upper optical depth. Special consideration of this stratum is justified, because there is good evidence that bio‐optical relationships are altered near the surface: (1) the fluorescence yield from chlorophyll declines, leading to bias in the estimation of pigment from fluorometry; (2) the modeled relationship between solar‐stimulated fluorescence and photosynthesis seems to deviate significantly from that presented for the lower euphotic zone; and (3) carbon‐specific and cellular attenuation cross sections of phytoplankton change substantially during exposures to bright light. Even the measurement of primary productivity is problematic near the sea surface, because vertical mixing is not simulated and artifactual inhibition of photosynthesis can result. These problems can be addressed by focusing more sampling effort, experimental simulation, and analytical consideration on the upper optical depth and by shortening timescales for the measurement of marine photosynthesis. Special efforts to study near‐surface processes are justified, because new bio‐optical algorithms will require quantitative descriptions of the responses of phytoplankton to bright light.
Cullen et al. (Sat,) studied this question.