Image Interpretation Color Composites Terra, July 6, 2002 Engel-Cox, J. et al. 2004. Atmospheric...
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Transcript of Image Interpretation Color Composites Terra, July 6, 2002 Engel-Cox, J. et al. 2004. Atmospheric...
![Page 1: Image Interpretation Color Composites Terra, July 6, 2002 Engel-Cox, J. et al. 2004. Atmospheric Environment.](https://reader036.fdocuments.net/reader036/viewer/2022062309/5697bf7b1a28abf838c83747/html5/thumbnails/1.jpg)
Image Interpretation
Color Composites
Terra, July 6, 2002 Engel-Cox, J. et al. 2004. Atmospheric Environment
![Page 2: Image Interpretation Color Composites Terra, July 6, 2002 Engel-Cox, J. et al. 2004. Atmospheric Environment.](https://reader036.fdocuments.net/reader036/viewer/2022062309/5697bf7b1a28abf838c83747/html5/thumbnails/2.jpg)
Information Content
• While scientists are primarily interested in geophysical quantities such as pollution concentrations and temperatures – space-borne sensors only measure radiances
• These radiances must be converted to geophysical quantities.
![Page 3: Image Interpretation Color Composites Terra, July 6, 2002 Engel-Cox, J. et al. 2004. Atmospheric Environment.](https://reader036.fdocuments.net/reader036/viewer/2022062309/5697bf7b1a28abf838c83747/html5/thumbnails/3.jpg)
Image Interpretation – Level 1
Radiances are converted to reflectances
![Page 4: Image Interpretation Color Composites Terra, July 6, 2002 Engel-Cox, J. et al. 2004. Atmospheric Environment.](https://reader036.fdocuments.net/reader036/viewer/2022062309/5697bf7b1a28abf838c83747/html5/thumbnails/4.jpg)
Image Interpretation – Level 1
Radiances are converted to temperature
![Page 5: Image Interpretation Color Composites Terra, July 6, 2002 Engel-Cox, J. et al. 2004. Atmospheric Environment.](https://reader036.fdocuments.net/reader036/viewer/2022062309/5697bf7b1a28abf838c83747/html5/thumbnails/5.jpg)
Color Composite
Yellow is a mix of red and green; orange is a mix of more red and some green; white is an equal mix of all three primaries, and black is simply the absence of any colored light of any wavelength
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Spectral Signatures
• Spectral signatures allow identification of classes (or features)
• Example : Water does not reflect beyond ~0.8 micron
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Imagery
Visible imageryClouds are whiteWater is black
Color CompositeClouds are whiteWater is black, Vegetation is green.
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Why is this important?
• You can only understand spectral signatures from Level 1 imagery
• This is the foundation for image classification, feature identification and understanding how to separate various classes.
• Example : How does one separate aerosols from clouds or the background?
![Page 9: Image Interpretation Color Composites Terra, July 6, 2002 Engel-Cox, J. et al. 2004. Atmospheric Environment.](https://reader036.fdocuments.net/reader036/viewer/2022062309/5697bf7b1a28abf838c83747/html5/thumbnails/9.jpg)
Image interpretation
• 550 nm imagery shows smoke, clouds, ocean and land
• Note that eye captures textural information as well
![Page 10: Image Interpretation Color Composites Terra, July 6, 2002 Engel-Cox, J. et al. 2004. Atmospheric Environment.](https://reader036.fdocuments.net/reader036/viewer/2022062309/5697bf7b1a28abf838c83747/html5/thumbnails/10.jpg)
Spectral Signatures of Aerosols and Clouds
MODIS Wavelength (um)
WaterClouds
MODIS Wavelength (um)
In thermal IR smoke andOcean temperatures aresame sub micron smoke does notEmit at these wavelengths.Clouds have colder temperatures
Smoke has sub micron size, thereforeNot reflective at 2.1 umWater clouds at 2.1 um reflect based on particle sizeOcean reflects less than smoke at 0.55um
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How to pick bands for Red, Green, Blue
• Depends upon your image• Example R : 645 nm, G : 865 nm, B : 645 nmNote that all of this is reflected solar radiationNote that 865 nm reflectance is in both the Red and Green and
Blue BandsSince the green is at 865 nm if there is healthy green vegetation
then then the color composite will show up as green for vegetation
Clouds are spectrally flat and reflect about the same in R, G, and B and therefore will be white
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Color Composites
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Fusing Level 1 and Level 2• AOD is a measure of the
extinction and scattering of light by particles in a total column from the satellite to the ground
• AOD is proportional to particulate concentration
• AOD is dimensionless; values typically range from 0 (clear, no haze) to 1 (very hazy, smoky, or dusty) in the US
• Clouds block the measurement of AOD!
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Next Steps
• In the afternoon session you will be ‘playing’ with GLIDER to interpret level 1B imagery
You will be creating this
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Other examples from Volcanic Ash
R, G, B = 0.47,0.55,0.65 um R,G,B = 0.65, 2.13, 11.0 um
ASH