• DocumentCode
    291755
  • Title

    Full wave scatter cross sections for two-dimensional random rough surfaces using joint conditional surface height characteristic functions

  • Author

    Bahar, Ezekiel ; Lee, Bom Son

  • Author_Institution
    Dept. of Electr. Eng., Nebraska Univ., Lincoln, NE, USA
  • Volume
    3
  • fYear
    1994
  • fDate
    8-12 Aug 1994
  • Firstpage
    1638
  • Abstract
    The bistatic radar scatter cross sections for two-dimensional random rough surfaces are obtained using the full wave approach. The formal solution is expressed as a 10-dimensional integral over the random surface heights h1, h2 and slopes h(x1), h x2, hz1, hz2 and the surface variables xs1, xx2, zs1, zz2. On averaging over the surface heights, the joint conditional surface height joint characteristic functions χ(a,blh(x1), hx2, hz1 , hz2) are introduced and the l0-dimensional integral reduces to an 8-dimensional integral. For homogeneous isotropic rough surfaces, χ is a function of rd=√(xd2+zd2 ) where xd≡xs1-xs2 and z d≡zx1-zx2 and the solution reduces to a 5-dimensional integral over h(x1), hx2, hz1 , hz2 and rd. If the radius of the curvature of the surface is large compared to the wavelength of the incident wave, the surface slopes at two neighboring points are approximately equal. Thus the 5-dimensional integral can be expressed as a 3-dimensional integral. These full wave results can be further simplified if the mean square surface slopes are small (≪0.15), in which case it can be assumed that the surface height and slopes are uncorrelated and the above 3-dimensional integral reduces to the product of a 2 and a 1-dimensional integral. In the low frequency limit when the surface height and slopes are of the same order of smallness, the full wave solution reduces to the small perturbation solution. For high frequencies, the 3-dimensional integral reduces to the 1-dimensional physical optics integral. In the high frequency limit, it reduces to the geometrical optics solution since in this case the Fourier transform of χ(a,b|hx,hz) is a Dirac delta function of the slopes at the specular points. In the illustrative examples, the full wave results are compared with the associated small perturbation and physical/geometrical optics results for a large range of frequencies
  • Keywords
    backscatter; electromagnetic wave scattering; geophysical techniques; radar applications; radar cross-sections; radar theory; remote sensing by radar; 10-dimensional integral; 3-dimensional integral; 5-dimensional integral; Dirac delta function; backscatter; bistatic radar scatter cross sections; formal solution; full wave approach; full wave scatter cross sections; geophysical measurement technique; joint conditional surface height characteristic functions; land surface terrain mapping; radar remote sensing; radar scattering theory; slope; specular point; two-dimensional random rough surface; Bistatic radar; Fourier transforms; Frequency; Geometrical optics; Optical surface waves; Physical optics; Radar scattering; Rough surfaces; Surface roughness; Surface waves;
  • fLanguage
    English
  • Publisher
    ieee
  • Conference_Titel
    Geoscience and Remote Sensing Symposium, 1994. IGARSS '94. Surface and Atmospheric Remote Sensing: Technologies, Data Analysis and Interpretation., International
  • Conference_Location
    Pasadena, CA
  • Print_ISBN
    0-7803-1497-2
  • Type

    conf

  • DOI
    10.1109/IGARSS.1994.399523
  • Filename
    399523