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Lecture 12: Image Processing
Thursday 11 February 2010 Lecture 12: Image Processing Reading Ch Last lecture: Earth-orbiting satellites
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Image Processing Because of the way most remote-sensing texts are organized, what strikes most students is the vast array of algorithms with odd names and obscure functions What is elusive is the underlying simplicity. Many algorithms are substantially the same – they have similar purposes and similar results
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Image Processing There are basically five families of algorithms that do things to images: Radiometric algorithms change the DNs Calibration Contrast enhancement 2) Geometric algorithms change the spatial arrangement of pixels or adjust DN’s based on their neighbors’ values Registration “Visualization” Spatial-spectral transformation Spatial filtering
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Image Processing 3) Spectral analysis algorithms are based on the relationship of DNs within a given pixel Color enhancement Spectral transformations (e.g., PCA) Spectral Mixture Analysis 4) Statistical algorithms characterize or compare groups of radiance data Estimate geophysical parameters Spectral similarity (classification, spectral matching) Input to GIS
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Image Processing 5) Modeling calculate non-radiance parameters from the radiance and other data Estimate geophysical parameters Make thematic maps Input to GIS
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Image Processing There is a dazzling array of things for the future professional to become familiar with I’m trying to over-simplify it to begin with Most algorithms are handled pretty well in most remote-sensing texts. Spectral Mixture Analysis is an exception, so… - we’ll look at Spectral Mixture Analysis next lecture
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Image Processing Sequence (single image)
Raw image data 1. Image display/inspection 2. Instrument calibration Image rectification, cartographic projection, registration, geocoding 3. Pre-processing 4. Atmospheric compensation 5. Pixel illumination-viewing geometry (topographic compensation) Working image data
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Image Processing Sequence (single image)
Working image data 6. Further image processing 7. Spectral analysis Selection of training data/endmembers 8. Processing Initial classification or other type of analysis 9. Interpretation/verification or further analysis 10. Product
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Band Ratios TITAN B/R G/R B/G Color Ratio Images
Commonly used ratios: - Landsat TM 5/7 for clays, carbonates, vegetation - 3/1 for iron oxide - 2/4 or 3/4 or 5/4 for vegetation CRC: R = B/R G = G/R B = B/G
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Ratios The Vegetation Index (VI) = DN4/DN3 is a ratio. Ratios suppress topographic shading because the cos(i) term appears in both numerator and denominator.
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NDVI Normalized Difference Vegetation Index
DN4-DN3 is a measure of how much chlorophyll absorption is present, but it is sensitive to cos(i) unless the difference is divided by the sum DN4+DN3.
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Principal Component Analysis (PCA)
Designed to reduce redundancy in multispectral bands Topography - shading Spectral correlation from band to band Either enhancement prior to visual interpretation or pre-processing for classification or other analysis Compress all info originally in many bands into fewer bands
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Principal Component Analysis (PCA)
In the simple case of 45º axis rotation, The rotation in PCA depends on the data. In the top case, all the image data have similar DN2/DN1 ratios but different intensities, and PC1 passes through the elongated cluster. In the bottom example, vegetation causes there to be 2 mixing lines (different DN4/DN3 ratios (and the “tasseled cap” distribution such that PC1 still passes through the centroid of the data, but is a different rotation that in the top case. PC1 PC2
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Tasseled Cap Transformation
Transforms (rotates) the data so that the majority of the information is contained in 3 bands that are directly related to physical scene characteristics Brightness (weighted sum of all bands – principal variation in soil reflectance) Greenness (contrast between NIR and VIS bands Wetness (canopy and soil moisture)
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Tasseled Cap Transformation (TCT)
TCT is a fixed rotation that is designed so that the mixing line connecting shadow and sunlit green vegetation parallels one axis and shadow-soil another. It is similar to the PCT. Soil Green
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Next lecture – Spectral Mixture Analysis
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