This article describes a method for determining the angular distribution of light polarization over a roughened surface of the sea. Our method relies on measurements of the Stokes vector elements using a polarization imaging camera that operates using the Division of Focal Plane (DoFP) method. It uses special monochrome CCD array in which the neighbouring cells, instead of recording different colours (red green and blue), are equipped with micropolarizers of four directions (0, 45, 90 and 135 degrees).We combined the camera with a fish-eye lens of Field of View (FoV) > 180 deg. Such a large FoV allowed us to crop out the fragment of the frame along the circular horizon, showing a view covering all directions of the hemisphere. Because of...
Above-water measurements of water-leaving radiance are widely used for water-quality monitoring and ...
Remote sensing has mainly relied on measurements of scalar radiance and its spectral and angular fea...
The upwelling spectral radiance distribution is polarized, and this polarization varies with the opt...
The spectral polarized radiance distribution provides the most complete description of the light fie...
The extent of plane polarised light resulting from Brewsters reflection from the wide-roughened sea...
The purpose of this article is to examine whether the change in single scattering albedo in the surf...
Mapping of marine benthic flora using remote sensing techniques has, over the past decade, been used...
Above-water radiometry depends on estimates of the reflectance factor rho of the sea surface to comp...
An imaging polarimetric slope sensing instrument for measuring water waves has been developed. From...
Retrieval of biogeochemical parameters from remotely sensed data in optically complex waters such as...
International audienceAirborne measurements of the linear polarization state of light were carried o...
Polarization states of the underwater light field were measured by a hyperspectral and multiangular ...
The article of record as published may be found at http://dx.doi.org/10.1117/12.825405The SALSA line...
This paper describes the design, construction and testing of a ship-borne spectroradiometer based on...
Above-water measurements of water-leaving radiance are widely used for water-quality monitoring and ...
Above-water measurements of water-leaving radiance are widely used for water-quality monitoring and ...
Remote sensing has mainly relied on measurements of scalar radiance and its spectral and angular fea...
The upwelling spectral radiance distribution is polarized, and this polarization varies with the opt...
The spectral polarized radiance distribution provides the most complete description of the light fie...
The extent of plane polarised light resulting from Brewsters reflection from the wide-roughened sea...
The purpose of this article is to examine whether the change in single scattering albedo in the surf...
Mapping of marine benthic flora using remote sensing techniques has, over the past decade, been used...
Above-water radiometry depends on estimates of the reflectance factor rho of the sea surface to comp...
An imaging polarimetric slope sensing instrument for measuring water waves has been developed. From...
Retrieval of biogeochemical parameters from remotely sensed data in optically complex waters such as...
International audienceAirborne measurements of the linear polarization state of light were carried o...
Polarization states of the underwater light field were measured by a hyperspectral and multiangular ...
The article of record as published may be found at http://dx.doi.org/10.1117/12.825405The SALSA line...
This paper describes the design, construction and testing of a ship-borne spectroradiometer based on...
Above-water measurements of water-leaving radiance are widely used for water-quality monitoring and ...
Above-water measurements of water-leaving radiance are widely used for water-quality monitoring and ...
Remote sensing has mainly relied on measurements of scalar radiance and its spectral and angular fea...
The upwelling spectral radiance distribution is polarized, and this polarization varies with the opt...