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Spectral attenuation and backscattering as indicators of average particle size
Applied Optics
|September 15, 2015
Summary
Ocean particle size distribution (PSD) can be estimated using spectral beam attenuation and backscattering coefficients. These optical measurements provide insights into particle characteristics, even when the PSD deviates from ideal models.
Area of Science:
- Ocean optics
- Particulate matter characterization
- Marine particle size distribution (PSD)
Background:
- Oceanic particulate beam attenuation and backscattering coefficients are spectrally dependent.
- The spectral slope of beam attenuation has been linked to the particle size distribution (PSD) slope.
- Recent advancements allow spectral backscattering measurements from various platforms, including space.
Purpose of the Study:
- To directly compare field-measured PSD with multispectral beam attenuation and backscattering coefficients.
- To investigate the relationship between spectral optical properties and PSD in a coastal bottom boundary layer.
- To assess the utility of backscattering measurements for inferring PSD shape.
Main Methods:
- Field measurements of particle size distribution (PSD).
- Multispectral measurements of beam attenuation coefficient.
- Multispectral measurements of backscattering coefficient.
Main Results:
- The spectral slope of beam attenuation correlated with average particle size, aligning with theoretical predictions for idealized PSD.
- Spectral backscattering measurements also reflected information about average particle size.
- This held true despite significant deviations of the measured PSD from a spectral power law shape.
Conclusions:
- Spectral beam attenuation is a reliable indicator of average particle size in oceanic environments.
- Spectral backscattering offers valuable information on particle size, even for non-ideal particle size distributions.
- These optical methods can enhance our understanding of marine particle characteristics.
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