4,654 research outputs found

    Degree and plane of polarization of multiple scattered light. 1: Homogeneous cloud layers

    Get PDF
    The degree of polarization and the direction of the plane of polarization are calculated by a Monte Carlo method for homogeneous layers. Two solar zenith angles and a range of optical thicknesses up to 10 are considered. The results are compared with calculations for single scattered photons. For a given pair of incident and scattered directions, there are only two possible values for the direction of the plane of polarization differing by 90 deg for single scattering from spherical aerosols. The choice between these two values depends only on the sign of the element M(-) in the first row and second column of the scattering matrix in the I, Q, U, V representation. In most cases there is little change in the direction of the plane of polarization when multiple scattering is taken into account, so that this quantity can usually be predicted from a very simple trigonometric relationship to good accuracy. Measurements of the direction of the plane of polarization at appropriately chosen angles provides information about the size distribution of the scattering centers

    Radiative transfer in realistic planetary atmospheres

    Get PDF
    The research accomplished during this period is briefly summarized. The interior radiances within an optically deep absorbing medium scattering according to the Haze L phase function is discussed along with a method for calculating the radiance and color of the twilight sky. The application of the matrix operator method to calculations of radiance, polarization, and ellipticity of the radiation scattered from homogeneous layers scattering is reported. Reports, and publications are listed

    Degree and plane of polarization of multiple scattered light. 2: Earth's atmosphere with aerosols

    Get PDF
    The degree of polarization, as well as the direction of the plane of polarization, were calculated by a Monte Carlo method for the reflected and transmitted photons from the earth's atmosphere. The solar photons were observed during multiple collisions with aerosols and the Rayleigh scattering centers in the atmosphere. The aerosol number density, as well as the ratio of aerosol to Rayleigh scattering, varies with height. The proportion of aerosol to Rayleigh scattering was appropriately chosen at each wavelength 0.4 microns and 0.7 microns; ozone absorption was included where appropriate. Three different aerosol number densities were used to study the effects of aerosol variations. Results are given for a solar zenith angle of 81.37 deg and a surface albedo of zero. The polarization of the reflected and transmitted photons was found to be sensitive to the amount of aerosols in the atmosphere at certain angles of observation

    Influence of single scattering albedo on reflected and transmitted light from clouds

    Get PDF
    Single scattering albedo effect on reflected and transmitted light from cloud

    Radiative transfer in realistic planetary atmospheres

    Get PDF
    Some 40 publications that appeared in scientific journals from 1973 to 1981 as well as 45 scientific reports issued during the grant period are listed by title. Topics cover the development of a matrix operator theory of radiative transfer which made possible the exact model calculations of the radiance as a function of height in planetary atmospheres; calculation of the Mie phase matrix for various types of particles as well as for radiance and polarization in planetary atmospheres; analysis of high dispersion spectroscopic observations of Venus; calculation of curves of growth for Venus; the development of a theory for calculating radiative transfer in spherical shell atmospheres; investigations of zonal winds on Venus; and examination of Rayleigh scattering

    Electromagnetic scattering from absorbing spheres

    Get PDF
    Electromagnetic scattering from absorbing sphere

    User Interface Panel with graphic LCD with touchscreen

    Get PDF
    Diplomová práce se zabývá realizací Panelu uživatelského rozhraní primárně určeného pro monitorování a zobrazování veličin elektrického pohonu experimentálního letounu Marabu. Panel je však možno použít v mnoha jiných náročných aplikacích. Důraz je kladen na seznámení s knihovnou funkcí pro grafické LCD.The Master`s thesis gives the basic facts about realisation of HMI. It will measure and display the electric quantity of electric traction of the Marabu experimental aircraft. The HMI is possible to use for other difficult applications. The main part of the thesis is overviewed the graphic function library for LCD.

    Reply to Bedi

    Get PDF

    Wage Compression as a Democratic Ideal

    Get PDF
    corecore