On the role of the seawater absorption-to-attenuation ratio in the radiance polarization above the southern Baltic surface

<p>Information about polarization of light leaving the ocean surface has the potential to improve the quality of bio-optical parameter retrieval from ocean color remote sensing (OCRS). This improvement can be applied in numerous ways, such as limiting of Sun glints and obtaining information ab...

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Main Authors: W. Freda, K. Haule, S. Sagan
Format: Article
Language:English
Published: Copernicus Publications 2019-06-01
Series:Ocean Science
Online Access:https://www.ocean-sci.net/15/745/2019/os-15-745-2019.pdf
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spelling doaj-86f7da073d3a45eb90df5df7ba800a422020-11-25T01:49:10ZengCopernicus PublicationsOcean Science1812-07841812-07922019-06-011574575910.5194/os-15-745-2019On the role of the seawater absorption-to-attenuation ratio in the radiance polarization above the southern Baltic surfaceW. Freda0K. Haule1S. Sagan2Department of Physics, Gdynia Maritime University, Gdynia, 81-225, PolandDepartment of Physics, Gdynia Maritime University, Gdynia, 81-225, PolandInstitute of Oceanology, Polish Academy of Sciences, Sopot, 81-712, Poland<p>Information about polarization of light leaving the ocean surface has the potential to improve the quality of bio-optical parameter retrieval from ocean color remote sensing (OCRS). This improvement can be applied in numerous ways, such as limiting of Sun glints and obtaining information about atmospheric aerosol properties for atmospheric correction as well as increasing the accuracy of the algorithms based on the water-leaving signal. Polarization signals at the top of the atmosphere (ToA) that include the water-leaving signal are strongly influenced by atmospheric molecular scattering and by direct Sun and sky reflections from the sea surface. For these reasons, it is necessary to better understand the factors that change the polarization of light in the atmosphere–ocean system, especially in coastal zones affected by dynamic changes. In this paper, the influence of seasonal variability of light absorption and scattering coefficients (inherent optical properties; IOPs) of seawater, wind speed and solar zenith angle (SZA) on the polarization of upwelling radiance over the sea surface in the visible light bands is discussed. The results come from a polarized radiative transfer model based on the Monte Carlo code and applied to the atmosphere–ocean system using averaged IOPs as input data. The results, presented in the form of polar plots of the total upwelling radiance degree of polarization (DoP), indicate that regardless of the wavelength of light and type of water, the highest value of the above-water DoP is strongly correlated with the absorption-to-attenuation ratio. The correlation is a power function that depends on both the SZA and the wind speed. The correlation versatility for different wavelengths of light is very unusual in optics of the sea and is therefore worth emphasizing.</p>https://www.ocean-sci.net/15/745/2019/os-15-745-2019.pdf
collection DOAJ
language English
format Article
sources DOAJ
author W. Freda
K. Haule
S. Sagan
spellingShingle W. Freda
K. Haule
S. Sagan
On the role of the seawater absorption-to-attenuation ratio in the radiance polarization above the southern Baltic surface
Ocean Science
author_facet W. Freda
K. Haule
S. Sagan
author_sort W. Freda
title On the role of the seawater absorption-to-attenuation ratio in the radiance polarization above the southern Baltic surface
title_short On the role of the seawater absorption-to-attenuation ratio in the radiance polarization above the southern Baltic surface
title_full On the role of the seawater absorption-to-attenuation ratio in the radiance polarization above the southern Baltic surface
title_fullStr On the role of the seawater absorption-to-attenuation ratio in the radiance polarization above the southern Baltic surface
title_full_unstemmed On the role of the seawater absorption-to-attenuation ratio in the radiance polarization above the southern Baltic surface
title_sort on the role of the seawater absorption-to-attenuation ratio in the radiance polarization above the southern baltic surface
publisher Copernicus Publications
series Ocean Science
issn 1812-0784
1812-0792
publishDate 2019-06-01
description <p>Information about polarization of light leaving the ocean surface has the potential to improve the quality of bio-optical parameter retrieval from ocean color remote sensing (OCRS). This improvement can be applied in numerous ways, such as limiting of Sun glints and obtaining information about atmospheric aerosol properties for atmospheric correction as well as increasing the accuracy of the algorithms based on the water-leaving signal. Polarization signals at the top of the atmosphere (ToA) that include the water-leaving signal are strongly influenced by atmospheric molecular scattering and by direct Sun and sky reflections from the sea surface. For these reasons, it is necessary to better understand the factors that change the polarization of light in the atmosphere–ocean system, especially in coastal zones affected by dynamic changes. In this paper, the influence of seasonal variability of light absorption and scattering coefficients (inherent optical properties; IOPs) of seawater, wind speed and solar zenith angle (SZA) on the polarization of upwelling radiance over the sea surface in the visible light bands is discussed. The results come from a polarized radiative transfer model based on the Monte Carlo code and applied to the atmosphere–ocean system using averaged IOPs as input data. The results, presented in the form of polar plots of the total upwelling radiance degree of polarization (DoP), indicate that regardless of the wavelength of light and type of water, the highest value of the above-water DoP is strongly correlated with the absorption-to-attenuation ratio. The correlation is a power function that depends on both the SZA and the wind speed. The correlation versatility for different wavelengths of light is very unusual in optics of the sea and is therefore worth emphasizing.</p>
url https://www.ocean-sci.net/15/745/2019/os-15-745-2019.pdf
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