Monte Carlo Calculations of the Polarization of Radiation in the Earth's Atmosphere-Ocean SystemSource: Journal of Physical Oceanography:;1973:;Volume( 003 ):;issue: 004::page 353DOI: 10.1175/1520-0485(1973)003<0353:MCCOTP>2.0.CO;2Publisher: American Meteorological Society
Abstract: The degree and direction of polarization, the ellipticity, and the radiance of the radiation at various levels in the atmosphere and ocean are calculated by a Monte Carlo method which includes all orders of multiple scattering. Both Rayleigh scattering by the molecules and Mie scattering by the aerosols, as well as molecular and aerosol absorption, are included in the model of the atmosphere. Similarly, in the ocean, both Rayleigh scattering by the water molecules and Mie scattering by the hydrosols, as well as absorption by the water molecules and hydrosols, are considered. Separate single-scattering phase matrices are calculated from Mie theory for the aerosols and hydrosols. Both the reflected and refracted rays, as well as the rays that undergo total internal reflection, are followed from the ocean surface which is assumed to be flat. The degree and direction of polarization, the ellipticity, the radiance and the flux are given as functions of the turbidity of the ocean, the solar zenith angle, and the wavelength of the radiation.
|
Collections
Show full item record
contributor author | Kattawar, George W. | |
contributor author | Plass, Gilbert N. | |
contributor author | Guinn, John A. | |
date accessioned | 2017-06-09T14:43:46Z | |
date available | 2017-06-09T14:43:46Z | |
date copyright | 1973/10/01 | |
date issued | 1973 | |
identifier issn | 0022-3670 | |
identifier other | ams-25390.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4162168 | |
description abstract | The degree and direction of polarization, the ellipticity, and the radiance of the radiation at various levels in the atmosphere and ocean are calculated by a Monte Carlo method which includes all orders of multiple scattering. Both Rayleigh scattering by the molecules and Mie scattering by the aerosols, as well as molecular and aerosol absorption, are included in the model of the atmosphere. Similarly, in the ocean, both Rayleigh scattering by the water molecules and Mie scattering by the hydrosols, as well as absorption by the water molecules and hydrosols, are considered. Separate single-scattering phase matrices are calculated from Mie theory for the aerosols and hydrosols. Both the reflected and refracted rays, as well as the rays that undergo total internal reflection, are followed from the ocean surface which is assumed to be flat. The degree and direction of polarization, the ellipticity, the radiance and the flux are given as functions of the turbidity of the ocean, the solar zenith angle, and the wavelength of the radiation. | |
publisher | American Meteorological Society | |
title | Monte Carlo Calculations of the Polarization of Radiation in the Earth's Atmosphere-Ocean System | |
type | Journal Paper | |
journal volume | 3 | |
journal issue | 4 | |
journal title | Journal of Physical Oceanography | |
identifier doi | 10.1175/1520-0485(1973)003<0353:MCCOTP>2.0.CO;2 | |
journal fristpage | 353 | |
journal lastpage | 372 | |
tree | Journal of Physical Oceanography:;1973:;Volume( 003 ):;issue: 004 | |
contenttype | Fulltext |