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Asymptotic optical depths in source-free ocean waters
Brian D Piening1, Norman J McCormick
1Department of Mechanical Engineering, University of Washington, Seattle, Washington 98195-2600, USA.
Applied Optics
|October 7, 2003
Summary
Ocean optics coefficients become independent of surface light conditions at specific depths. These depths vary based on water properties and incident illumination, crucial for solving inverse problems in underwater optics.
Area of Science:
- Ocean optics
- Radiative transfer theory
- Inherent optical properties (IOPs)
Background:
- Underwater light fields are influenced by surface illumination and water properties.
- Asymptotic regime describes light field behavior at depth, independent of surface conditions.
- Understanding the transition to the asymptotic regime is key for accurate optical modeling.
Purpose of the Study:
- To determine the depth at which key diffuse optical properties become independent of surface incident illumination.
- To investigate how incident light characteristics and water IOPs affect this depth.
- To provide insights for solving inverse ocean optics problems assuming an asymptotic light field.
Main Methods:
- Analysis of depth dependence for downward diffuse attenuation coefficient.
- Examination of upward-to-downward plane irradiance ratio depth profiles.
- Calculation of vertically upward radiance-to-downward plane irradiance ratio and mean cosine of radiance.
Main Results:
- Identified specific depths where diffuse attenuation, irradiance ratios, and mean cosine become insensitive to surface illumination.
- Demonstrated that these depths are significantly influenced by the spectral characteristics of incident light.
- Showed a strong dependence on the inherent optical properties (IOPs) of the water column.
Conclusions:
- The depth at which the light field approaches its asymptotic state is not fixed but depends on illumination and water IOPs.
- This finding is critical for validating models and algorithms in underwater remote sensing and optical oceanography.
- Accurate estimation of these transition depths improves the reliability of inverse problem solutions in ocean optics.