• DocumentCode
    1017778
  • Title

    Frequency and azimuthal variations of radar cross section and their influence upon low-frequency SAR imaging

  • Author

    Axelsson, Sune R.J.

  • Author_Institution
    Nat. Defence Res. Establ., Linkoping, Sweden
  • Volume
    33
  • Issue
    5
  • fYear
    1995
  • fDate
    9/1/1995 12:00:00 AM
  • Firstpage
    1258
  • Lastpage
    1265
  • Abstract
    Low-frequency SAR requires a highly extended synthetic aperture to give a spatial resolution comparable to that of a microwave SAR. As a result, the azimuth angle of the target is varying significantly along the synthetic aperture path. The signal-bandwidth to carrier-frequency ratio is also much larger compared to conventional microwave SAR, giving a fluctuating target response over the frequency band occupied by the transmitted signal. In this paper, the variations of the radar response with frequency and observation angle and their effects upon SAR imaging are analyzed for Mie-scattering spheres and flat plates. The influence of a reflecting sea or ground surface below the target is also discussed
  • Keywords
    airborne radar; backscatter; geophysical techniques; radar cross-sections; radar detection; radar imaging; radar polarimetry; remote sensing by radar; search radar; spread spectrum radar; synthetic aperture radar; 20 to 90 MHz; CARABAS; HF radar; Mie-scattering sphere; VHF radar; azimuth angle; azimuthal variation; carrier-frequency ratio; flat plate; geophysical measurement technique; highly extended synthetic aperture; land surface; low frequency SAR imaging; radar cross section; radar remote sensing; radar scattering; signal-bandwidth; stepped frequency radar; synthetic aperture radar; terrain mapping; Azimuth; Frequency; Image analysis; Radar cross section; Radar imaging; Radar polarimetry; Sea surface; Soil; Spaceborne radar; Synthetic aperture radar;
  • fLanguage
    English
  • Journal_Title
    Geoscience and Remote Sensing, IEEE Transactions on
  • Publisher
    ieee
  • ISSN
    0196-2892
  • Type

    jour

  • DOI
    10.1109/36.469490
  • Filename
    469490