A novel approach to the polarization correction of spaceborne spectrometers

[1] We present a new polarization correction algorithm for polarization sensitive spaceborne spectrometers like Global Ozone Monitoring Experiment (GOME) or Scanning Imaging Absorption Spectrometer for Atmospheric Cartography (SCIAMACHY). These instruments measure polarization with less spectral resolution than the radiance. As a consequence, the current GOME polarization correction algorithm allows radiance errors of 10% in the UV and 3% in the visible (VIS) and near-IR. Using simulated spectra, we show that the continuum Stokes elements Q and U over a large wavelength range (300 to 800 nm) can be reliably retrieved from only a limited set of measurements (three to five). The interpolation to other wavelengths is made using numerically calculated polarization spectra. These polarization spectra can be calculated for Rayleigh scattering atmospheres, but we show that the retrieval is just as effective for cloudy and aerosol scenes as for clear scenes. For GOME the remaining radiance errors are less than 3% (UV) and 1% (VIS, near-IR), and often smaller than 0.5%. The lack of actual UV (300–330 nm) polarization measurements prevents further reduction of the radiance errors. We also show how the ozone Huggins absorption band may be accounted for through a parameterization and a single polarization broadband measurement and that strong but narrow absorption bands like the O2A band maybe ignored without detrimental effect on the algorithm.

[1]  Bruce W. Fitch Effects of reflection by natural surfaces on the radiation emerging from the top of the earth's atmosphere , 1981 .

[2]  Florence Nadal,et al.  Parameterization of surface polarized reflectance derived from POLDER spaceborne measurements , 1999, IEEE Trans. Geosci. Remote. Sens..

[3]  M. Buchwitz,et al.  SCIAMACHY: Mission Objectives and Measurement Modes , 1999 .

[4]  Maurice Herman,et al.  Polarization of light reflected by crop canopies , 1991 .

[5]  H. V. Hulst Light Scattering by Small Particles , 1957 .

[6]  J. Hovenier,et al.  The polarized internal radiation field of a planetary atmosphere , 1989 .

[7]  W. D. Rooij,et al.  Expansion of Mie scattering matrices in generalized spherical functions , 1984 .

[8]  Donald K. Perovich,et al.  Observations of the polarization of light reflected from sea ice , 1998 .

[9]  Michael Eisinger,et al.  The Global Ozone Monitoring Experiment (GOME): Mission Concept and First Scientific Results , 1999 .

[10]  P. J. Curran,et al.  Remote sensing using partially polarized light , 1986 .

[11]  J. Hovenier,et al.  The adding method for multiple scattering calculations of polarized light , 1987 .

[12]  Piet Stammes,et al.  Improving the polarization correction algorithm of GOME (Global Ozone Monitoring Experiment) , 1999, Optics + Photonics.

[13]  F. X. Kneizys,et al.  AFGL atmospheric constituent profiles (0-120km) , 1986 .

[14]  Paul J. Curran,et al.  A photographic method for the recording of polarised visible light for soil surface moisture indications , 1978 .

[15]  Jean-Claude Roger,et al.  Polarization of the solar light scattered by the earth-atmosphere system as observed from the U.S. shuttle , 1994 .

[16]  J. Hovenier,et al.  Detecting radiances in the O2 A band using polarization sensitive satellite instruments with application to Global Ozone Monitoring Instrument , 2000 .

[17]  N. Schutgens,et al.  Parametrisation of Earth's polarisation spectrum in the ultra-violet ☆ , 2002 .

[18]  J. Hovenier,et al.  A fast method for simulating observations of polarized light emerging from the atmosphere applied to the oxygen-A band , 2000 .

[19]  D. E. Bowker,et al.  Spectral reflectances of natural targets for use in remote sensing studies , 1985 .

[20]  William L. Smith,et al.  IRS 2000: CURRENT PROBLEMS IN ATMOSPHERIC RADIATION , 2000 .