High Angular Resolution Measurements of the Anisotropy of Reflectance of Sea Ice and Snow

©2018. American Geophysical Union. We introduce a new method to determine the anisotropy of reflectance of sea ice and snow at spatial scales from 1 m 2 to 80 m 2 using a multispectral circular fish-eye radiance camera (CE600). The CE600 allows measuring radiance simultaneously in all directions of...

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Published in:Earth and Space Science
Main Authors: Goyens, C., Marty, S., Leymarie, E., Antoine, David, Babin, M., Bélanger, S.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2018
Subjects:
Online Access:https://hdl.handle.net/20.500.11937/66405
https://doi.org/10.1002/2017EA000332
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spelling ftcurtin:oai:espace.curtin.edu.au:20.500.11937/66405 2023-06-11T04:16:33+02:00 High Angular Resolution Measurements of the Anisotropy of Reflectance of Sea Ice and Snow Goyens, C. Marty, S. Leymarie, E. Antoine, David Babin, M. Bélanger, S. 2018 restricted https://hdl.handle.net/20.500.11937/66405 https://doi.org/10.1002/2017EA000332 unknown http://hdl.handle.net/20.500.11937/66405 doi:10.1002/2017EA000332 Journal Article 2018 ftcurtin https://doi.org/20.500.11937/6640510.1002/2017EA000332 2023-05-30T19:52:04Z ©2018. American Geophysical Union. We introduce a new method to determine the anisotropy of reflectance of sea ice and snow at spatial scales from 1 m 2 to 80 m 2 using a multispectral circular fish-eye radiance camera (CE600). The CE600 allows measuring radiance simultaneously in all directions of a hemisphere at a 1° angular resolution. The spectral characteristics of the reflectance and its dependency on illumination conditions obtained from the camera are compared to those obtained with a hyperspectral field spectroradiometer manufactured by Analytical Spectral Device, Inc. (ASD). Results confirm the potential of the CE600, with the suggested measurement setup and data processing, to measure commensurable sea ice and snow hemispherical-directional reflectance factor, HDRF, values. Compared to the ASD, the reflectance anisotropy measured with the CE600 provides much higher resolution in terms of directional reflectance (N = 16,020). The hyperangular resolution allows detecting features that were overlooked using the ASD due to its limited number of measurement angles (N = 25). This data set of HDRF further documents variations in the anisotropy of the reflectance of snow and ice with the geometry of observation and illumination conditions and its spectral and spatial scale dependency. Finally, in order to reproduce the hyperangular CE600 reflectance measurements over the entire 400-900 nm spectral range, a regression-based method is proposed to combine the ASD and CE600 measurements. Results confirm that both instruments may be used in synergy to construct a hyperangular and hyperspectral snow and ice reflectance anisotropy data set. Article in Journal/Newspaper Sea ice Curtin University: espace Earth and Space Science 5 1 30 47
institution Open Polar
collection Curtin University: espace
op_collection_id ftcurtin
language unknown
description ©2018. American Geophysical Union. We introduce a new method to determine the anisotropy of reflectance of sea ice and snow at spatial scales from 1 m 2 to 80 m 2 using a multispectral circular fish-eye radiance camera (CE600). The CE600 allows measuring radiance simultaneously in all directions of a hemisphere at a 1° angular resolution. The spectral characteristics of the reflectance and its dependency on illumination conditions obtained from the camera are compared to those obtained with a hyperspectral field spectroradiometer manufactured by Analytical Spectral Device, Inc. (ASD). Results confirm the potential of the CE600, with the suggested measurement setup and data processing, to measure commensurable sea ice and snow hemispherical-directional reflectance factor, HDRF, values. Compared to the ASD, the reflectance anisotropy measured with the CE600 provides much higher resolution in terms of directional reflectance (N = 16,020). The hyperangular resolution allows detecting features that were overlooked using the ASD due to its limited number of measurement angles (N = 25). This data set of HDRF further documents variations in the anisotropy of the reflectance of snow and ice with the geometry of observation and illumination conditions and its spectral and spatial scale dependency. Finally, in order to reproduce the hyperangular CE600 reflectance measurements over the entire 400-900 nm spectral range, a regression-based method is proposed to combine the ASD and CE600 measurements. Results confirm that both instruments may be used in synergy to construct a hyperangular and hyperspectral snow and ice reflectance anisotropy data set.
format Article in Journal/Newspaper
author Goyens, C.
Marty, S.
Leymarie, E.
Antoine, David
Babin, M.
Bélanger, S.
spellingShingle Goyens, C.
Marty, S.
Leymarie, E.
Antoine, David
Babin, M.
Bélanger, S.
High Angular Resolution Measurements of the Anisotropy of Reflectance of Sea Ice and Snow
author_facet Goyens, C.
Marty, S.
Leymarie, E.
Antoine, David
Babin, M.
Bélanger, S.
author_sort Goyens, C.
title High Angular Resolution Measurements of the Anisotropy of Reflectance of Sea Ice and Snow
title_short High Angular Resolution Measurements of the Anisotropy of Reflectance of Sea Ice and Snow
title_full High Angular Resolution Measurements of the Anisotropy of Reflectance of Sea Ice and Snow
title_fullStr High Angular Resolution Measurements of the Anisotropy of Reflectance of Sea Ice and Snow
title_full_unstemmed High Angular Resolution Measurements of the Anisotropy of Reflectance of Sea Ice and Snow
title_sort high angular resolution measurements of the anisotropy of reflectance of sea ice and snow
publishDate 2018
url https://hdl.handle.net/20.500.11937/66405
https://doi.org/10.1002/2017EA000332
genre Sea ice
genre_facet Sea ice
op_relation http://hdl.handle.net/20.500.11937/66405
doi:10.1002/2017EA000332
op_doi https://doi.org/20.500.11937/6640510.1002/2017EA000332
container_title Earth and Space Science
container_volume 5
container_issue 1
container_start_page 30
op_container_end_page 47
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