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Role of measurement uncertainties in observed variability in the spectral backscattering ratio: a case study in mineral-rich coastal waters

Role of measurement uncertainties in observed variability in the spectral backscattering ratio: a case study in mineral-rich coastal waters
Role of measurement uncertainties in observed variability in the spectral backscattering ratio: a case study in mineral-rich coastal waters
The particulate backscattering ratio (bbp=bp) is a useful indicator of the angular scattering characteristics
of natural waters. Recent studies have shown evidence both for and against significant spectral variability
in bbp=bp in the visible domain, but most show significant variability in its magnitude. We present
results from a case study in which both backscattering and scattering coefficients were measured at nine
wavelengths in a region of UK coastal waters where optical scattering is strongly influenced by inorganic
particles and where a wide range of turbidities is found in a small geographic area. Using a new approach
based on regression analysis of in situ signals, it is shown that, for this study site, most of the apparent
variability in the magnitude of the backscattering ratio can be attributed to measurement uncertainties.
Regression analysis suggests that bbp=bp is wavelength dependent for these mineral-rich waters. This
conclusion can only be avoided by positing the existence of undocumented, systematic, wavelengthdependent
errors in backscattering measurements made by two independently calibrated sensors. These
results are important for radiative transfer simulations in mineral-dominated waters where the backscattering
ratio has often been assumed to be spectrally flat. Furthermore, spectral dependence also has
profound implications for our understanding of the relationship between bbp=bp and particle size
distributions in coastal waters since the commonly assumed power-law distribution is associated with
a spectrally flat particulate backscattering ratio for nonabsorbing particles.
0003-6935
4663-4675
McKee, David
62c5fe4f-030c-4236-8ccb-f992ca247ef4
Chami, Malik
f7a24b2f-84a7-4ab9-bd93-1de9bcd5acff
Brown, Ian
42b64387-e5bb-4729-9b46-4bc79d749688
Sanjuan Calzado, Violeta
f9ccf1a7-545b-4041-8fe6-e388c2905859
Doxaran, David
b1b19eb1-131c-4881-8afd-d1c81d94f5ff
Cunningham, Alex
2d172388-9e7e-4cb2-9fe7-ff34b283efd1
McKee, David
62c5fe4f-030c-4236-8ccb-f992ca247ef4
Chami, Malik
f7a24b2f-84a7-4ab9-bd93-1de9bcd5acff
Brown, Ian
42b64387-e5bb-4729-9b46-4bc79d749688
Sanjuan Calzado, Violeta
f9ccf1a7-545b-4041-8fe6-e388c2905859
Doxaran, David
b1b19eb1-131c-4881-8afd-d1c81d94f5ff
Cunningham, Alex
2d172388-9e7e-4cb2-9fe7-ff34b283efd1

McKee, David, Chami, Malik, Brown, Ian, Sanjuan Calzado, Violeta, Doxaran, David and Cunningham, Alex (2009) Role of measurement uncertainties in observed variability in the spectral backscattering ratio: a case study in mineral-rich coastal waters. Applied Optics, 48 (24), 4663-4675. (doi:10.1364/AO.48.004663).

Record type: Article

Abstract

The particulate backscattering ratio (bbp=bp) is a useful indicator of the angular scattering characteristics
of natural waters. Recent studies have shown evidence both for and against significant spectral variability
in bbp=bp in the visible domain, but most show significant variability in its magnitude. We present
results from a case study in which both backscattering and scattering coefficients were measured at nine
wavelengths in a region of UK coastal waters where optical scattering is strongly influenced by inorganic
particles and where a wide range of turbidities is found in a small geographic area. Using a new approach
based on regression analysis of in situ signals, it is shown that, for this study site, most of the apparent
variability in the magnitude of the backscattering ratio can be attributed to measurement uncertainties.
Regression analysis suggests that bbp=bp is wavelength dependent for these mineral-rich waters. This
conclusion can only be avoided by positing the existence of undocumented, systematic, wavelengthdependent
errors in backscattering measurements made by two independently calibrated sensors. These
results are important for radiative transfer simulations in mineral-dominated waters where the backscattering
ratio has often been assumed to be spectrally flat. Furthermore, spectral dependence also has
profound implications for our understanding of the relationship between bbp=bp and particle size
distributions in coastal waters since the commonly assumed power-law distribution is associated with
a spectrally flat particulate backscattering ratio for nonabsorbing particles.

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Published date: 20 August 2009

Identifiers

Local EPrints ID: 71768
URI: http://eprints.soton.ac.uk/id/eprint/71768
ISSN: 0003-6935
PURE UUID: 5a0ea4c8-6b7a-4c16-978f-96de06ae2dd8

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Date deposited: 22 Dec 2009
Last modified: 13 Mar 2024 20:42

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Contributors

Author: David McKee
Author: Malik Chami
Author: Ian Brown
Author: Violeta Sanjuan Calzado
Author: David Doxaran
Author: Alex Cunningham

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