Volume 45 Issue 3
Apr.  2016
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Xia Runqiu, Wang Xia, Jin Weiqi, Liang Jian'an, Liu Jing. Distance model of infrared polarization imaging system used in sea-surface environment[J]. Infrared and Laser Engineering, 2016, 45(3): 304007-0304007(5). doi: 10.3788/IRLA201645.0304007
Citation: Xia Runqiu, Wang Xia, Jin Weiqi, Liang Jian'an, Liu Jing. Distance model of infrared polarization imaging system used in sea-surface environment[J]. Infrared and Laser Engineering, 2016, 45(3): 304007-0304007(5). doi: 10.3788/IRLA201645.0304007

Distance model of infrared polarization imaging system used in sea-surface environment

doi: 10.3788/IRLA201645.0304007
  • Received Date: 2015-07-05
  • Rev Recd Date: 2015-08-10
  • Publish Date: 2016-03-25
  • The fact that infrared radiation of sea surface is polarized has been proved by many experiments. Searching and detecting ability of infrared polarization imaging systems in sea-surface environment was a major concern for polarization imaging research. Sea surface was realized by using a statistical model of oceanographic literature which originated from the spectrum for long and short wind-driven waves proposed by Eifouhaily. A Monte Carlo reverse ray-tracing method was used to investigate the behavior of mid/long-wave infrared Stokes radiance which included the information of radiance intensity, degree of polarization and angle of polarization, at the realized wind roughed sea surface. The minimum resolvable temperature difference(MRTD) parameters for Stokes-vector components were proposed based on standard error propagation method. Finally, detectable range of infrared polarization imaging used in sea surface environment was analyzed by comparing apparent-temperature differences(ATD) between target and sea background with the MRTD of Stokes-vector components.
  • [1] Cox Charles, Walter Munk. Measurement of the roughness of the sea surface from photographs of the sun's glitter[J]. JOSA, 1954, 44(11):838-850.
    [2] Elfouhaily T, Chapron B, Katsaros K, et al. A unified directional spectrum for long and short wind-driven waves[J]. Journal of Geophysical Research:Oceans, 1997, 102(C7):15781-15796.
    [3] Nicholas R Nalli, William L Smith, Bormin Huang. Quasi-specular model for calculating the reflection of atmospheric-emitted infrared radiation from a rough water surface[J]. Applied Optics, 2001, 40(9):1343-1353.
    [4] Tessendorf, Jerry. Simulating Nature:Realistic and Interactive Techniques Simulating Ocean Water[M]. New York:Special Interest Group on Computer Graphics, 2001.
    [5] Apel John R. An improved model of the ocean surface wave vector spectrum and its effects on radar backscatter[J]. Journal of Geophysical Research:Oceans, 1994, 99(C8):16269-16291.
    [6] Schott, John Robert. Fundamentals of polarimetric remote sensing[C]//SPIE Press, 2009, 81:38-40.
    [7] Bevington, Philip R, D Keith Robinson. Data Reduction and Error Analysis for the Physical Sciences[M]. New York:McGraw-Hill, 1969:39-49.
    [8] Berdahl, Paul, Richard Fromberg. The thermal radiance of clear skies[J]. Solar Energy, 1982, 29(4):299-314.
    [9] Zou Xiaofeng, Wang Xia, Jin Weiqi, et al. Atmospheric effectsonin frared polarization imaging system[J]. Infrared and Laser Engineering, 2012, 41(2):304-308. (in Chinese)
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Distance model of infrared polarization imaging system used in sea-surface environment

doi: 10.3788/IRLA201645.0304007
  • 1. School of Optoelectronics,Beijing Institute of Technology,Key Laboratory of Photoelectronic Imaging Technology and System,Ministry of Education of China,Beijing 100081,China

Abstract: The fact that infrared radiation of sea surface is polarized has been proved by many experiments. Searching and detecting ability of infrared polarization imaging systems in sea-surface environment was a major concern for polarization imaging research. Sea surface was realized by using a statistical model of oceanographic literature which originated from the spectrum for long and short wind-driven waves proposed by Eifouhaily. A Monte Carlo reverse ray-tracing method was used to investigate the behavior of mid/long-wave infrared Stokes radiance which included the information of radiance intensity, degree of polarization and angle of polarization, at the realized wind roughed sea surface. The minimum resolvable temperature difference(MRTD) parameters for Stokes-vector components were proposed based on standard error propagation method. Finally, detectable range of infrared polarization imaging used in sea surface environment was analyzed by comparing apparent-temperature differences(ATD) between target and sea background with the MRTD of Stokes-vector components.

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