Remote Sensing


Geog 483/553
Fall 2009 
Tu Th 2:00am - 3:20pm
352 Fillmore 
Instructor: Ling Bian 
Office: 120 Wilkeson Quad
Office hours: Tu Th 12:30-1:30pm or by appt
TA:  Heath Robinson
Lab Tu 12:30-1:50pm, W145
       F   9:30-10:50am  W145   


Radar Remote Sensing
use synthetic aperture principle

SEASAT SAR 1978
        - designed to observe ocean waves, sea ice, and coastlines
        - 800km orbit, 25m range and azimuth resolutions,
          l=23.5cm, HH, 20-26o look angle
        - the fine resolution required high transmission rate
        - data were only acquired when satellite was in the sight of
            the ground station

Shuttle Image Radar-A (SIR-A) 1981
        - a synthetic aperture radar carried by the Shuttle
            Transportation System
        - designed to observe land information
        - 260km altitude, 40m range and azimuth resolutions,
          l=23.5cm, HH, fixed large look angle (47-53)

Shuttle Image Radar-B (SIR-B) 1984
        - l=23.5cm, HH, 25m azimuth resolution, 15-45m range resolution
        - varied look angle 15-60o to acquire stereo images
        - obtain roughness and moisture info at different look angles

Shuttle Image Radar-C (SIR-C) 1994
        - multiple radar bands l=23.5, 5.8, 3.1cm, color composite
        - varied look angle 15-60o, HH, HV, VV, and VH
          25m azimuth resolution, 15-45m range resolution

        - ocean: waves, wind motion, current motion, and sea ice,
            ecosystems: land use, vegetation, fire effects, flood,
                                and clear cutting
            hydrology: water, wetland, soil moisture, snow and glacier
            geology: geologic structures, soil erosion, transportation,
                                and deposition, active volcanoes
            rain and clouds

ALMAZ-1 1991
        Soviet Union satellite radar system
        - 300km orbit, l=10cm, HH, varied look angle 20-70o,
          10-30m range and azimuth resolutions

ERS-1, ERS-2,
        European Space Agency, 1991, 1995
        - sun-synchronous orbit, 785km
        - 16 ~ 18 days temporal resolution
        - three sensor systems including a C-band active microwave
            instrumentation with 30m resolution, VV, 23o look angle

ENVISAT-1
        European Space Agency, 2002
        - Advanced Synthetic Aperture Radar (ASAR)
        - 30m resolution, 14-45o look angle

JERS-1
        National Development Agency of Japan, 1992
        - sun-synchronous orbit, 568km
        - a four-band optical sensor
        - 23cm L band SAR, HH, 18m resolution, 35o look angle

ALOS
        National Development Agency of Japan
        Advanced land Observing Satellite (ALOS)
        - a Phased Array L-band Synthetic Aperture Radar system
        - varied look angle and multi-polarization

RADARSAT
        Canadian Space Agency, 1995
        - designed to observe sea ice, coastal line, land cover,
            agriculture, and forest
        - 798km orbit, 1-3days, l=5.6cm, HH
        - various spatial resolutions and look angles
 

Interferometric Radar
        - based on the phase difference of radar signals received by
            antennas located at different positions in space
        - with a known interferometric baseline, the phase difference
            is used to calculate elevation
        - single-pass interferometry: two antennas on a single
            aircraft
        - repeat-pass interferometry: single antenna with multiple
            passes

        Shuttle Radar Topography Mission (SRTM)
        - single-pass interferometry
        - covers 60oN-56oS, 30m resolution DEM, C and X bands
 

LIDAR
        LIght Detection And Ranging
        uses pulses of laser light directed toward the ground and measured
        return time to measure distances
        - rapid pulsing
        - can record up to five returns per pulse, thus
            discriminating multiple surfaces per pulse
        - equipped with GPS, recorded data are georeferenced
        - large quantity of data
        - used for generating DEMs, contours, and feature extraction

        Ice, Cloud, and Land Elevation Satellite (ICESat) 2003

         - NASA’s Earth Observing System (EOS)
         - NIR and visible
         - collects precise measurements of the mass balance of polar ice sheets

        Vegetation Canopy Lidar (VCL), the first mission of NASAs Earth
                System Science Pathfinder (ESSP) program
        - measure ground surface and canopy-top elevation, vertical
            distribution of canopy elements
        - no longer actively developed

Reading; chpt 8
 
 
 
 
 
 
 

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