Back to Search Start Over

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

Authors :
Marcel Babin
C. Goyens
David Antoine
Edouard Leymarie
Simon Bélanger
S. Marty
Université du Québec à Rimouski (UQAR)
Laboratoire d'océanographie de Villefranche (LOV)
Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut de la Mer de Villefranche (IMEV)
Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)
Takuvik Joint International Laboratory ULAVAL-CNRS
Université Laval [Québec] (ULaval)-Centre National de la Recherche Scientifique (CNRS)
Source :
Earth and Space Science, Earth and Space Science, American Geophysical Union/Wiley, 2018, 5 (1), pp.30-47. ⟨10.1002/2017EA000332⟩
Publication Year :
2018
Publisher :
American Geophysical Union (AGU), 2018.

Abstract

International audience; We introduce a new method to determine the anisotropy of reflectance of sea ice and snow at spatial scales from 1 m2 to 80 m2 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.

Details

ISSN :
23335084
Volume :
5
Database :
OpenAIRE
Journal :
Earth and Space Science
Accession number :
edsair.doi.dedup.....b9d0868c8aabfaa1ec8c8c8ca97e7d86
Full Text :
https://doi.org/10.1002/2017ea000332