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Remote Sensing ' Lecture 7

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Near Polar orbiting earth. resources satellites: SPOT. LIDAR. Remote Sensing .... Lecture 7 ... and after 3 years in orbit the satellite stopped functioning ... – PowerPoint PPT presentation

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Title: Remote Sensing ' Lecture 7


1
Lecture 7 Content
  • Near Polar orbiting earth
  • resources satellites
  • SPOT
  • LIDAR

2
  • SPOT
  • LANDSAT system suffered three major drawbacks
  • Very high ground resolution is not possible with
    the mechanical MSS used
  • The repetition time for any one scene is quite
    long, 18 or 16 days per satellite. Satellites
    have limited operational value especially when
    data is needed for monitoring purposes.
  • Stereoscopic viewing is only possible in narrow
    image overlaps, and the accuracy of height
    estimation is low

3
  • SPOT
  • French tackled these drawbacks as follows
  • It was decided to use a pushbroom scanner. Not
    only can modern pushbroom scanners provide high
    resolution, they have a longer and more reliable
    life expectancy, lower power requirements, and
    higher geometric and radiometric accuracy
  • Mirrors make off-nadir viewing possible which
    allow any area to be viewed frequently. Oblique
    viewing allowed for stereoscopic viewing

4
  • SPOT satellite characteristics
  • SPOT in the first earth resource satellite to be
    launched from Europe
  • Other characteristics of SPOT which are similar
    to LANDSAT
  • Near-polar sun synchronous orbit
  • Transmission of data to ground stations with the
    possibility of on-board recording
  • SPOT sensors can sense in high resolution (10m)
    panchromatic mode or lower resolution (20m)
    multispectral mode in 3 wavelengths

5
  • A single SPOT scene covers a geographical
  • area of 60 x 60 km.
  • Two alternative modes of imaging are possible
    using
  • SPOT
  • Panchromatic black and white, with a ground
  • resolution of 10 m
  • Multispectral colour, with 20 m ground
  • resolution acquired simultaneously in 3 bands
  • green, red and near infrared.

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8
  • In a MSS it scans the scene from side to side and
    reflects radiation from the ground surface onto a
    detector
  • This process is limited by the accuracy of the
    rotating mirror
  • To overcome this problem a HRV (High Resolution
    Visible) scanner is used in SPOT. It does not
    have any moving parts, instead, it records each
    scan line at one go by means of a line of
    detectors one detector for each area sampled on
    the ground
  • Detectors are controlled by a microchip and
    controls 1,728 detectors on SPOT

9
  • Comparison between pushbroom scanner and MSS

10
  • SPOT 1 and SPOT 2 available and launched in 1985
    and 1986 respectively
  • SPOT 1 carry two identical pushbroom scanners
    which are called High Resolution Visible (HRV)
    scanners
  • When in panchromatic mode all of the detectors
    are sampled with a spatial resolution of 10m
  • Used for mapping scales of 1150,000 to 1100,000
  • When in multispectral mode only half of the
    detectors are sampled with a spatial resolution
    of 20m
  • Used for pollution monitoring to vegetation
    mapping

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14
SPOT ground receiving stations
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17
SPOT Panchromatic
18
SPOT Multispectral
19
  • LIDAR
  • Light Detection And Ranging (LIDAR)
  • It is a radiometer system that uses a light beam
    in stead of a microwave radar beam (Radar) to
    obtain measurements of speed, altitude, direction
    and range of a target
  • Lidars are used to precisely measure distances
    and properties of far-away objects
  • Its operation is that a powerful laser transmits
    a short and intense pulse of light
  • Very high spatial resolution, for example a DEM
    was created of a complete coverage of the
    Netherlands at a spatial resolution of 1 cm
    (Introduction to LIDAR, 1997).

20
  • Use of LIDAR for accurate determination of
    terrain elevations began in the late 1970s but
    their use was limited due to project
    cost-effectiveness
  • One of the most successful early applications of
    LIDAR was in the determination of accurate water
    depths
  • Modern LIDAR acquisition makes use of a rapidly
    pulsing (20,000 to 50,000 pulses/sec) laser and a
    highly accurate clock to measure time
  • The principle of LIDAR is similar to that of
    RADAR
  • Further details in lecture 10

21
LIDAR image at ground zero NY
22
  • Lidar Applications
  • Atmospheric science
  • - dynamics measurements temperatures, winds,
    and waves- climate measurements clouds,
    aerosols, and water vapor- ozone measurements
    depletions and polar stratospheric clouds- high
    altitude trace metal measurements sodium and
    potassium- pollution monitoring
  • Astronomy
  • planetary surface relief mapping (eg lidar Mars
    maps by NASA)
  • Topographic mapping
  • erosion monitoring
  • Bathymetry (under water mapping)
  • harbor profiling for marine safety

23
  • Forest ground and canopy measurements
  • used to assess forest growth and health
  • Building and factory construction
  • measurements allow for precise prefabrication,
    improving efficiency and reducing costs
  • Mine shaft mapping
  • allows cavern monitoring for worker safety
  • Aircraft docking
  • for safe aircraft maneuvering near airport
    terminals
  • Automobile speed monitoring
  • a replacement for hand-held radar guns

24
  • The End
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