Notes
Slide Show
Outline
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Radar Remote Sensing
  • Nick Faust
  • GTRI/EOSL
  • 404-894-0021
  • Nick.faust@gtri.gatech.edu
  • Source from Nick Short:
  • http://rst.gsfc.nasa.gov/Sect8/Sect8_1.html
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Radar Definition
  • Radio Detection and Ranging (RADAR)
  • Microwave and Millimeter Wavelengths
  • Active System
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Types of RADAR
  • Fixed site
    • Air Traffic, Naval, weather, etc
  • Airborne Imaging
    • Side Looking Airborne Radar (SLAR)
    • Synthetic Aperture Radar (SAR)
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Weather Radar – Indiana 96
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Imaging Resolution
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SAR Theory
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SAR Theory 2
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Radar Phenomenology
  • Response is due to:
    • Surface roughness
    • Dielectric constant
    • Angle of incidence
    • Polarization
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Radar Frequencies/Wavelengths
  • Ka Band: Frequncy 40,000-26,000 MHz; Wavelength (0.8-1.1 cm)
  • K Band: 26,500-18,500 MHz; (1.1-1.7 cm)
  • X Band: 12,500-8,000 MHz; (2.4-3.8 cm)
  • C Band: 8,000-4,000 MHz; (3.8-7.5 cm)
  • L Band: 2,000-1,000 MHz; (15.0-30.0 cm)
  • P Band: 1,000- 300 MHz; (30.0-100.0 cm)
  • Source GSFC-Nick Short
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RADAR Advantages
  • Day or Night Capability
  • Can See Through Clouds
  • Military and Civilian Applications
  • High Resolution Imaging
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Radar Disadvantages
  • Requires more On-Board Power (Active)
  • Coherent system – Intensity Speckle
  • Geometric Distortions
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Rwanda Landsat
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SIRC Rwanda
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New Orleans – SIR C
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Los Angeles - SIRC
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Sahara Desert – SIRC Penetration