Linear Polarization
Document Sample


Polarization
Ben Kravitz
Thursday, September 10, 2009
2
Outline
• What polarization is
• How it works
• How it is useful to remote sensing
Orientation
QuickTime™ and a
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are neede d to se e this picture.
http://www.colorado.edu/physics/2000/polarization/polarizationII.html
Ray direction remains the
Polarization
http://www.colorado.edu/physics/2000/polarization/images/typicalLIght.jpg
Polarized Light
Typical Light
http://www.colorado.edu/physics/2000/polarization/images/polarizeLight.jpg
Orientation (again)
Recall that, no matter which way the ray is oriented, we can
break up the light ray vector into its horizontal and vertical
components
Polarizing Filters
http://www.colorado.edu/physics/2000/polarization/polarizationII.html
Examples
http://www.colorado.edu/physics/2000/polarization/bloc
king_light.html
http://www.colorado.edu/physics/2000/polarization/twis
ting_light.html
Uses of Polarization
• Satellite transmission (multiple channels per
frequency)
• Minimize interference
• Different responses by surfaces to different
polarizations
Polarization and Remote
Sensing
http://www.ccrs.nrcan.gc.ca/glossary/index_e.php?id=2818
Different orientations are scattered in different ways
Linear Polarization
• Vertical Transmit, Vertical Receive (VV) - scattering due to surface
capillary waves has a higher signal-to-noise ratio for this polarization,
commonly used in oceanography for extracting surface wind speeds
• Horizontal Transmit, Horizontal Receive (HH) - studying soil moisture
(horizontally polarized waves pass through vegetation into the soil
below), good for separating ice from water, good for ship detection
• Horizontal Transmit, Vertical Receive (HV) - retrieval depends on the
scattering mechanism, so good for differentiating different types of
materials or structures
• Vertical Transmit, Horizontal Receive (VH) - same as HV, but receiver
noise is different, so this is averaged with HV to get a less noisy
measurement
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