Abstract

Commonly we see the diffuse attenuation coefficient of downwelling irradiance (Kd) expressed as a sum of the contributions of various constituents. We show here that, both theoretically and numerically, because Kd is an apparent optical property, this approach is not consistent with radiative transfer. We further advocate the application of models of Kd developed in past decades that are not only consistent with radiative transfer but also provide more accurate estimates, in particular for coastal turbid waters.

Highlights

  • Solar radiation is the energy source for the entire earth system

  • Since the variation of Ed(0−) is independent of water properties (except extremely turbid waters where the enhanced upwelling flux will result in significant contributions to Ed(0−) due to internal reflection), it is imperative to describe the variation of Kd for various aquatic environments when quantifying the impact of water constituents on the heat budget (Morel and Antoine, 1994; Ohlmann et al, 2000), the feedback of oceanic systems on climate changes (Rochford et al, 2001; Gnanadesikan and Anderson, 2009), as well as the vertical variation of primary production (Sathyendranath and Platt, 1995)

  • The contributions of colored dissolved organic matter (CDOM) and organic detritus are considered as co-varying with phytoplankton, and lumped into the Kbio term

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Summary

Frontiers in Marine Science

AOPs Are Not Additive: On the Biogeo-Optical Modeling of the Diffuse Attenuation Coefficient. We see the diffuse attenuation coefficient of downwelling irradiance (Kd) expressed as a sum of the contributions of various constituents. Both theoretically and numerically, because Kd is an apparent optical property (AOP), this approach is not consistent with radiative transfer. We further advocate the application of models of Kd developed in past decades that are consistent with radiative transfer and provide more accurate estimates, in particular for coastal turbid waters

BACKGROUND
THEORETICAL MODEL OF Kd
NUMERICAL DEMONSTRATION
Findings
CONCLUSIONS
Full Text
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