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 coloured square The University of Melbourne   Geology (Engineering Course)

 Remote Sensing

 

 

This page includes the outline text from the classroom PowerPoint presentation, together with selected graphics from that presentation. The graphics will appear when the title hotlink is activated.

A copy of the classroom presentation, in .pdf format, can be downloaded from here.
Textbooks referred to are:

McLean and Gribble: Geology for Civil Engineers; [NB this segment is not represented in MG.]
Dennen and Moore: Geology and Engineering (DM)
Waltham: Foundations of Engineering Geology (W)
Lillesand and Kiefer: Remote Sensing and Image Interpretation

Portions of this display are illustrated with images from Small Blue Planet - The electronic Satellite Atlas, from Now What Software.


Remote Sensing



Remote Sensing
The science and art of obtaining information about an object, area, or phenomenon through the analysis of data acquired by a device that is not in contact with the object, area, or phenomenon under investigation.

Usual Interpretation
  • Use of electromagnetic spectrum
    • near-visible part of spectrum
    • surface-imaging techniques
  • Broad definition includes most/all of Geophysics, but normally considered separate field

Advantage of scale
  • Uniformity of image over large areas confers advantage for some applications
  • Example is enhanced, low-visible-light (night-time) image of Antarctica from satellite platform
  • Literal snapshot of weather pattern

Antarctic DMSP Image

Photography and Beyond
Device Camera Sensor
Recording Medium Film Electronic
Processing Chemical Computing
Product Photograph Imagery
Display Stereoscope Screen/Print
Interpretation Human!

Physical Mechanism
  • Source - Sun (blackbody radiator)
  • Spectrum at detector is altered by
    • Transmission losses
      • scattering, absorption
    • Reflection losses at surface
    • Scattering losses at surface
  • Last two are source of information

Source energy spectra

Surface Interactions
  • Energy may be reflected, transmitted, or absorbed by materials making up surface
    • reflection depends on composition of surface
  • Energy may be diffused by rough surface
    • diffusion depends on scale of roughness

General comparison

Information Content
  • Different materials respond differently across spectrum - including beyond-visible
  • Additional information available in infra-red, thermal, radar bands of spectrum
  • All these (and black-and-white) might be used if appropriate

Surface Interactions
  • Both Physics and Geometry affect response
  • "Ground Truth" establishes effect on spectrum in particular area
  • Ground Truth work very important, because actual spectrum is usually a composite

Response overview



Basic Example
  • Next image is natural-colour image of volcano
  • Surface/rock colours show texture from topography
  • Little discrimination possible

Stromboli - "natural colour"

Stromboli - Infra-red image

Infra-Red enhancement
  • Distinctive colour change
  • Information from IR band displayed as "Red" colour
  • Explanation needs ground investigation
    • (probably younger lava flows, weathering differences)

Imaging System Classes
Common Imaging System Types:
  • Airborne Photography
    • b/w, colour, near infra-red
  • Airborne Imagery
    • thermal infra-red, radar
  • Satellite Imagery
  • colour, near infra-red, thermal infra-red, radar

Satellite Imaging
  • Light reflected/diffused from individual area ("pixel") 10-80 m square focussed on individual detector, through filter
  • Detector output is electronic, digital
  • Each pixel may drive multiple filter/detector channels

Satellite Imaging
  • Aperture scanned to build up image (compare TV)
  • Image reconstructed by computer/camera system
  • Separate image possible for each channel (that is, each filtered part of spectrum)

Image Presentation
  • Image displayed in "false colour"
  • Red, Green, Blue colours assigned to selected channels and mixed
  • Choice of channel depends on application
  • More complex imaging possible

Landsat Thematic Mapper

(Thanks to Daniel Pérez for supplying a correction to this screen).


Brazil - Thematic Mapper

Land-Use Monitoring
  • Brazil example shows resolution using false-colour
"blue" is recent clearing
"orange" is recent regrowth
"red" is old-growth forest
  • Evaluation is consistent across scene

Mineral spectra

Further false-colour example
  • Next visual page shows
"blue" (near-IR) snow
"red" (thermal band) basalt outcrop
"green" vegetation
"purple" (mid-IR) agriculture

Iceland - Thematic Mapper

Thermal Mapping
  • Direct measurement of surface temperature possible
  • Resolution to fractions of Celsius degree is possible
  • Information may come from temperature distribution itself
  • Heat capacity (strongly dependent on water content) also mappable from thermal information

Example of thermal mapping
  • Hunters Point Power Station, CA
  • Land image from Thematic Mapper bands 1, 2, 3
  • Water image from IR band 8
  • Image shows distribution of heated wastewater from power station (temperature range < 5 Celsius degrees).

Example of thermal mapping

Primary radiation
  • Radiometer measures energy radiated from surface
  • Version of thermal band on Landsat TM satellite
  • Next image is mosaic, shows response of Advanced Very High Resolution Radiometer
  • Unsubtle changes due to change in conditions for different parts of mosaic

SE Australia - AVHRR


Radiometric Response Mapping

  • Response images radioactive minerals (K as red, U as blue, Th as green) in top cms of soil
  • Spatial resolution to tens of metres, unaffected by weather, vegetation
  • Can be directly relevant to soil, terrain types and conditions



 

 

Created: 30 June, 1999
Last modified:
Authorised by: Head, School of Earth Sciences

Maintained by: Lindsay Thomas, School of Earth Sciences.
Email: thomas@unimelb.edu.au