radar remote sensing
DESCRIPTION
Radar Remote Sensing. RADAR => RA dio D etection A nd R anging. Radar Remote Sensing. Active remote sensing system using 1 cm to 1m wavelengths (microwaves). Microwave Atmospheric Window. Radar Systems. AIRSAR - Flies in DC-8 with C, L, and P bands - PowerPoint PPT PresentationTRANSCRIPT
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Radar Remote Sensing
• RADAR => RAdio Detection And Ranging
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Radar Remote Sensing• Active remote sensing system using 1 cm to 1m wavelengths
(microwaves).
Band Wavelength Interval (cm)
Ka 0.8 to 1.1
K 1.1 to 1.7
Ku 1.7 to 2.4X 2.4 to 3.8C 3.8 to 7.5
S 7.5 to 15L 15 to 30
P 30 to 100
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Microwave Atmospheric Window
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Radar Systems
• AIRSAR - Flies in DC-8 with C, L, and P bands• SRTM (Shuttle Radar Topography Mission) - X-band and C-band radar
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Radar Applications
• Radar imaging– Measure returned energy flux– Return controlled by dielectric constant (index of refraction) of
materials, roughness of surface at wavelength scale, and slopes
• Radar altimetry– Measure round trip travel time to determine distance between
antenna and surface• Radar interferometry
– Broadcast from one antenna and receive at another antenna with known distance between them
– Phase difference for two antennas used to determine topography.
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Characteristics of Radar Images
• SLAR - Side-Looking Airborne Radar• SAR - Synthetic Aperture Radar (also side-looking)• Side-looking characteristics induce some geometric effects quite
distinct from framing cameras.
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Depression and Incidence Angle
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Characteristics of Radar Images• Radar records strength of returned signal and round trip travel
time to determine pixel brightness and location of pixel perpendicular to flight direction, respectively.
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Radar Remote Sensing
• Radar Image Characteristics– Shadows– Foreshortening– Layover– Relief Displacement
• Radar Spatial Resolution– Cross Track or Range Resolution– Along Track Resolution
• SLAR• SAR
)(30)(
)(30)(
cmGhz
Ghzcm
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Radar Image Characteristics
• For side-looking radar systems, position within an image line is determined by travel time of radar beam.
• Multiple image lines are created by forward motion of aircraft or satellite.
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Radar Shadows• Radar shadows occur when slopes are not seen by radar beam.
That is, when slope angle is greater than the depression angle.• Shadow lengths get longer behind obstacles as depression angle
gets smaller.
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Radar Shadows• For simple terrain (flat with bumps), shadows can be used to get
heights. • See diagram below. H = aircraft altitude, h = feature height,
Rr = slant range to far end of shadow, Rs = slant range length of shadow.
• Distances measured on slant range image.
r
s
r
s
RRHh
RR
Hh
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Slant Range and Ground Range Images
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Foreshortening• Given that range determines cross-track pixel location, there is
geometric foreshortening.• Cross-track length of feature determines how long it remains in
radar illumination.• If surface slope is normal to wave front, then slope appears as a
point in output image.• Foreshortening is one reason
why radar is side-looking.Features directly beneathaircraft would have same return times andthus show as single point.
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Foreshortening Example
• Seasat image of Alaska. Radar illumination is from the top.
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Foreshortening
• Surfaces seen with largest depression angles (closest to antenna) will have greatest amount of foreshortening.
• Foreshortening decreases as the depression angle decreases (i.e., further from antenna) for a given surface slope.
• Example of foreshortening for slopes of 15º from horizontal.
DepressionAngle
Foreshortening(fore slope)
Foreshortening(back slope)
75 0.0 (point) 0.5055 0.34 0.7745 0.50 0.8725 0.77 0.9815 0.87 1.00 (true
length)2
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Layover in Radar Images
• Layover occurs when slopes are steep that for return from top of slope is received before the return from the bottom of slope.
• Object appears to be "laying over" on its side in the radar image.• Layover increases as depression angle increases.
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Layover Example
• Seasat image of Alaska. Radar illumination is from the top.
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Layover Example
• Mount Fujiyama, Japan. Radar illumination from the top.
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Radar Image Spatial Resolution• Separate values of resolution for the along-track and cross-track
directions.• Consider cross-track or range resolution.• Range resolution dependent on pulse length, t, and on
depression angle, b. Not dependent on antenna altitude.• Two features will be resolved in the range direction if their return
pulses do not arrive back at the antenna at the same time.
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Range Resolution
• Pulse length in distance is t*c.• Assume that features are separated in
range direction if horizontal separation(Rr
),is greater than (t*c)/2.
• From the triangle in diagram, we canderive range resolution (Rr).
• As pulse length and depression angledecrease, the range resolution gets smaller.Better resolution further from the antenna.
• As depression angle increase for points closerto the antenna, range resolution is worse.
• Another reason why radar can not image directlybeneath the antenna.
bt
t
b
cos2
2cos
cR
AndR
c
r
r
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Along-Track Resolution
• Along-track resolution in independent of the range resolution.• For simple SLAR system, the along-track cell size (Ra)is dependent
on beam width projected onto the ground. Beam width and thus along-track resolution becomes wider for distances further from the antenna.
• Where S is slant range, is radarwavelength, and D is antenna width.
• Equation is derived from fact that beamwidth is proportional to /D.
• For SAR systems, a longer antennais synthesized for greater slant rangesto maintain a constant along-trackresolution.
DSRa