Revisiting the role of oceanic phase function in remote sensing reflectance

The effect of angular structure differences between measured and best-fit analytical phase functions of the equivalent backscattering ratio on calculated reflectance values was studied and shown to be significant. We used a Monte Carlo radiative transfer code to check the effect of choosing differen...

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Main Authors: Włodzimierz Freda, Jacek Piskozub
Format: Article
Language:English
Published: Elsevier 2012-01-01
Series:Oceanologia
Subjects:
Online Access:http://www.iopan.gda.pl/oceanologia/54_1.html#A2
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author Włodzimierz Freda
Jacek Piskozub
author_facet Włodzimierz Freda
Jacek Piskozub
author_sort Włodzimierz Freda
collection DOAJ
description The effect of angular structure differences between measured and best-fit analytical phase functions of the equivalent backscattering ratio on calculated reflectance values was studied and shown to be significant. We used a Monte Carlo radiative transfer code to check the effect of choosing different analytical (several Fournier-Forand (1994) and Henyey-Greenstein (1941)) phase functions with backscattering ratios identical to the "classical" average Petzold function. We show that the additional variability of the resulting water leaving radiance is about 7% (4% between the Fournier-Forand functions themselves) for most scenarios. We also show a~previously unknown maximum of the discrepancy (up to 10%) for highly scattering waters. We discuss the importance of relative differences in phase function for different angular ranges to this maximum and to the behaviour of the discrepancy as a function of solar zenith angle.
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spelling doaj.art-aa105ec1c60a4eb3a9ded3bf6492ec9e2022-12-21T20:39:17ZengElsevierOceanologia0078-32342012-01-015412938Revisiting the role of oceanic phase function in remote sensing reflectanceWłodzimierz FredaJacek PiskozubThe effect of angular structure differences between measured and best-fit analytical phase functions of the equivalent backscattering ratio on calculated reflectance values was studied and shown to be significant. We used a Monte Carlo radiative transfer code to check the effect of choosing different analytical (several Fournier-Forand (1994) and Henyey-Greenstein (1941)) phase functions with backscattering ratios identical to the "classical" average Petzold function. We show that the additional variability of the resulting water leaving radiance is about 7% (4% between the Fournier-Forand functions themselves) for most scenarios. We also show a~previously unknown maximum of the discrepancy (up to 10%) for highly scattering waters. We discuss the importance of relative differences in phase function for different angular ranges to this maximum and to the behaviour of the discrepancy as a function of solar zenith angle.http://www.iopan.gda.pl/oceanologia/54_1.html#A2Marine opticsPhase functionsRemote sensing reflectanceScattering
spellingShingle Włodzimierz Freda
Jacek Piskozub
Revisiting the role of oceanic phase function in remote sensing reflectance
Oceanologia
Marine optics
Phase functions
Remote sensing reflectance
Scattering
title Revisiting the role of oceanic phase function in remote sensing reflectance
title_full Revisiting the role of oceanic phase function in remote sensing reflectance
title_fullStr Revisiting the role of oceanic phase function in remote sensing reflectance
title_full_unstemmed Revisiting the role of oceanic phase function in remote sensing reflectance
title_short Revisiting the role of oceanic phase function in remote sensing reflectance
title_sort revisiting the role of oceanic phase function in remote sensing reflectance
topic Marine optics
Phase functions
Remote sensing reflectance
Scattering
url http://www.iopan.gda.pl/oceanologia/54_1.html#A2
work_keys_str_mv AT włodzimierzfreda revisitingtheroleofoceanicphasefunctioninremotesensingreflectance
AT jacekpiskozub revisitingtheroleofoceanicphasefunctioninremotesensingreflectance