Physical and optical parameters within the atmosphere-ocean system have been retrieved by a multiple scattering analysis of the reflectance and degree of linear polarization data measured by the airborne POLDER sensor in Medimar campaign in 1991. Assuming an atmosphere-ocean system with a Cox-Munk type rough sea surface model, the theoretical reflectance and -degree of linear polarization were computed by the doubling and adding method for several different models. In this study the retrieval was made by assuming a fixed refractive index of the aerosol particles, i.e., Nr=1.33-0.0i. We obtained several important results in this study as follows:
1) By comparing computed results with the observed data at 0.85
2) The reflectance data analysis in the perpendicular plane rejected an isotropic Cox-Munk model, but it indicated that an anisotropic Cox-Munk model should be used in the sea surface wind field retrieval.
3) The surface wind speed was estimated to be 10.0m/sec
4) Further study should be made for other refractive indices of the aerosol particles. More refinement of the present multiple scattering code to include upwelling polarization components from below the sea surface is also necessary.
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Akihiro YAMAZAKI, Yoshiyuki KAWATA, "Physical and Optical Parameter Retrieval from Airborne POLDER Data" in IEICE TRANSACTIONS on Communications,
vol. E78-B, no. 12, pp. 1598-1603, December 1995, doi: .
Abstract: Physical and optical parameters within the atmosphere-ocean system have been retrieved by a multiple scattering analysis of the reflectance and degree of linear polarization data measured by the airborne POLDER sensor in Medimar campaign in 1991. Assuming an atmosphere-ocean system with a Cox-Munk type rough sea surface model, the theoretical reflectance and -degree of linear polarization were computed by the doubling and adding method for several different models. In this study the retrieval was made by assuming a fixed refractive index of the aerosol particles, i.e., Nr=1.33-0.0i. We obtained several important results in this study as follows:
1) By comparing computed results with the observed data at 0.85
2) The reflectance data analysis in the perpendicular plane rejected an isotropic Cox-Munk model, but it indicated that an anisotropic Cox-Munk model should be used in the sea surface wind field retrieval.
3) The surface wind speed was estimated to be 10.0m/sec
4) Further study should be made for other refractive indices of the aerosol particles. More refinement of the present multiple scattering code to include upwelling polarization components from below the sea surface is also necessary.
URL: https://global.ieice.org/en_transactions/communications/10.1587/e78-b_12_1598/_p
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@ARTICLE{e78-b_12_1598,
author={Akihiro YAMAZAKI, Yoshiyuki KAWATA, },
journal={IEICE TRANSACTIONS on Communications},
title={Physical and Optical Parameter Retrieval from Airborne POLDER Data},
year={1995},
volume={E78-B},
number={12},
pages={1598-1603},
abstract={Physical and optical parameters within the atmosphere-ocean system have been retrieved by a multiple scattering analysis of the reflectance and degree of linear polarization data measured by the airborne POLDER sensor in Medimar campaign in 1991. Assuming an atmosphere-ocean system with a Cox-Munk type rough sea surface model, the theoretical reflectance and -degree of linear polarization were computed by the doubling and adding method for several different models. In this study the retrieval was made by assuming a fixed refractive index of the aerosol particles, i.e., Nr=1.33-0.0i. We obtained several important results in this study as follows:
1) By comparing computed results with the observed data at 0.85
2) The reflectance data analysis in the perpendicular plane rejected an isotropic Cox-Munk model, but it indicated that an anisotropic Cox-Munk model should be used in the sea surface wind field retrieval.
3) The surface wind speed was estimated to be 10.0m/sec
4) Further study should be made for other refractive indices of the aerosol particles. More refinement of the present multiple scattering code to include upwelling polarization components from below the sea surface is also necessary.
keywords={},
doi={},
ISSN={},
month={December},}
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TY - JOUR
TI - Physical and Optical Parameter Retrieval from Airborne POLDER Data
T2 - IEICE TRANSACTIONS on Communications
SP - 1598
EP - 1603
AU - Akihiro YAMAZAKI
AU - Yoshiyuki KAWATA
PY - 1995
DO -
JO - IEICE TRANSACTIONS on Communications
SN -
VL - E78-B
IS - 12
JA - IEICE TRANSACTIONS on Communications
Y1 - December 1995
AB - Physical and optical parameters within the atmosphere-ocean system have been retrieved by a multiple scattering analysis of the reflectance and degree of linear polarization data measured by the airborne POLDER sensor in Medimar campaign in 1991. Assuming an atmosphere-ocean system with a Cox-Munk type rough sea surface model, the theoretical reflectance and -degree of linear polarization were computed by the doubling and adding method for several different models. In this study the retrieval was made by assuming a fixed refractive index of the aerosol particles, i.e., Nr=1.33-0.0i. We obtained several important results in this study as follows:
1) By comparing computed results with the observed data at 0.85
2) The reflectance data analysis in the perpendicular plane rejected an isotropic Cox-Munk model, but it indicated that an anisotropic Cox-Munk model should be used in the sea surface wind field retrieval.
3) The surface wind speed was estimated to be 10.0m/sec
4) Further study should be made for other refractive indices of the aerosol particles. More refinement of the present multiple scattering code to include upwelling polarization components from below the sea surface is also necessary.
ER -