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Study Guide for Final Geography 418/518, Fundamentals of Remote Sensing |
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| The revolutionary potential of high spatial resolution hyperspectral (HSRH) imagery is exemplified by the Probe1 1-m minimum noise fraction image of the Lamar River, WY, which provides a detailed map of wood (red), and variations in water depth and turbulence (blues), sediment size (purples to blues), brush (green), and canopy (yellow). In contrast, the simulated Landsat TM5 image of the same site barely distinguishes river bottom from surrounding regions. |
The second midterm covers weeks 6 through 10 of lecture, lab and readings.
Note: materials below are guide to what was covered in lectures and text book, but not the articles or workbook.
As with the first midterm, when you study for the test, focus first on lecture notes. You should also pay close attention to the text materials from your labs. The book will once again be an important source of information to fill in gaps in your understanding. In particular, you will want to use the book to fill in several topics that were not covered in lecture (e.g., conversion of DNs to absolute radiance values, a number of the classification topics). In the case of the lab materials, you should understand the broad concepts, do not worry about remembering details about the software (e.g., which sequence of commands to enter in order to access the polynomial rectification procedures, although you should know what polynomial rectification is).
The following is a list of points that you should put particular emphasis into studying. Although I try to make the list as comprehensive as possible, there may be a question or two on the test that this list doesn't cover. By in large, however, if you have a good grasp on the definitions, facts, concepts and skills below, you will do well on the test.
I. The Remote Sensing System (yes, we did this before, but I want you to remember this overarching framework)
Energy Sources
passive
active
the electromagnetic spectrum
Energy Movement through the Atmosphere
Absorption
Scattering
Reflection
Transmission
Energy/Matter Interactions at Earth's Surface
Absorption
Scattering
Reflection
Transmission
Sensor Systems and Platforms
Data Handling Systems
Data User
II. The Electromagnetic Spectrum (ditto the comment above)
Wavelengths associated with:
ultraviolet light
visible light (blue, green, and red)
photographic infrared (IR)
near IR
shortwave IR
midrange IR
thermal IR
radar
Range and intensity of wavelengths
emitted from the sun
emitted from the earth
be able to draw a diagram showing the two key points above, with wavelengths and names of different ranges of energy
III. Major Components of Image Processing Covered in this Class
Data Restoration - the "fixing" of the data
Image Enhancement - better visualization of key features or processes
Image Classification - making a map of categories
IV. Data Restoration/Image Preprocessing
Image Rectifications (geometric corrections)
Sources of distortion/error
Systematic (be able to give some examples)
Non-systematic (be able to give examples)
Techniques for adjusting pixel locations
Mathematical corrections for systematic errors
models for earth rotation, scanner characteristics
camera focal adjustments
Approaches for systematic/nonsystematic error
polynomial approaches
use of ground control points
how different order polynomials
use of root mean square (RMS) error for evaluation
triangulation/rubber sheeting approaches (requires same input as polynomial approaches)
orthorectification techniques (requires DEM)
reasons for choosing one of three approaches for rectifying image
Techniques for assigning pixel values to the new locations
Nearest neighbor sampling
Bilinear interpolation
Cubic convolution
Advantages/disadvantages
of each approach
Radiometric Corrections (atmospheric corrections)
Atmospheric scattering
"Relative corrections" based on information from the image, i.e. relative to the image
Haze removal (subtract lowest value - a poor approach)
Contrast stretch where lowest digital value assigned to zero (better, but still weak)
Regression of NIR vs Visible wavelengths to determine lowest value to subtract (better, but still weak)
"Absolute corrections" (i.e. correction applied independent of image data)
physical models based on atmospheric data (e.g., MODTRAN, ATREM, etc.)
Solar corrections
Relative correction for comparing one image to another, or part of same image with different illumination
comparison of same target or identical targets on both images to adjust reflectance values
Absolute corrections
for variations in Earth/Sun distance
for sun angle ("sun elevation" in the book)
Bidirectional Reflectance
No unique and relatively error-free solutions at this time
Conversion of DNs to absolute radiance values
When it is important to do this
How this is accomplished
Equipment Distortion (included in noise category in the text book)
Line dropout and cosmetic "fixes"
Sensor miscalibration (line striping) and approaches for correcting
Noise Removal
Use of moving windows (kernels) to detect and correct noise
V. Image Enhancement
Point Operators (Radiometric Enhancements)
Masks (termed "gray-level thresholding" in the book)
Level slicing
Contrast stretches
Basic concept of how contrast stretches work
Some different kinds of contrast stretches
Local Operators (Spatial Filters)
Concept of "convolution," which is use of moving windows called "kernels"
High frequency filters ("sharpens" image)
Low frequency filters ("blurs" image)
Directional and non-directional filters
Multi-Image or Multi-Band Enhancements (know the general concepts and when one might use the techniques below)
True color composites
False color composites
Intensity-hue-saturation color space transformations
3-D image drape
Band ratioing (called "spectral ratioing" in book)
to remove topographic illumination effects
vegetation indices
Principal components/canonical analysis
to reduce spectral redundancy
key features that are illuminated
The tasseled cap transformation
Fourier transforms (note: book
includes this as a spatial operation and it can be used this way.
But it can also be used to examine variations in frequencies across
bands)
VI. Classification
Supervised Classification (know general concept and advantages/disadvantages of each approach)
Overall approach
selection of spectral training sites
Training sites should represent a particular spectral signature. One feature (e.g. water) may have several different spectral signatures (e.g., turbid/clear; shallow/deep)
preferably the training sites should be scattered across the image
training sites should be "pure" and not represent a mix of spectral signatures
number of training pixels per category should be a minimum of 10 times total number of categories (but preferably higher)
spectral signature of training sites can come from:
imagery (top down approach)
ground based spectral measurements
training site refinement
use of histograms and coincident spectral plots
quantitative indices (e.g. transformed divergence, Jeffries-Matusita distance)
ability of training pixels to correctly classify themselves (self classification)
Algorithms for classification
Minimum distance
Parallelepiped
Gaussian maximum likelihood classifier
Unsupervised Classification
Cluster concept
Use of unsupervised classification:
to assess range of land cover in the image
as a guide to selecting training sites for subsequent supervised classification
to provide insights into range of spectral variations and their spatial distributions and extents (to see the landscape with a new eye)
Post-Classification
Combining classes
Majority filters
Multi-image refinem,ents (e.g., adding a DEM)\
Mixed Pixel Classification
Linear mixing/unmixing
Fuzzy classifications
Accuracy Assessment
Error matrix (also called a confusion matrix or a contingency table)
Producer's accuracy
User's accuracy
Error of omission
Error of commission
KHAT statistic
Development of validation data sets to create error matrix
Validation data should not be same pixels as training sites
Minimum 50 validation sites (could be pixels), more if large area or many categories
Validation data should be from around image, not just one location (e.g., 50 pixels from one site is not appropriate)
VI. Hyperspectral Imagery
How hyperspectral differs from multispectral
Applications
Spectral matching to spectral libraries
Pixel unmixing (spectral mixing)
Spectral angle mappings as a classifier
VII. Active Systems (Chapter 7)
Principles of Active Radar
Radar = Radio Detection and Ranging
Wavelengths
K band, 0.8-2.4 cm
X band, 2.4-3.8 cm
C band, 3.8-7.5 cm
S band, 7.5-15 cm
L band, 15-30 cm
Major types of radar instruments
Plan Position Indicator (PPI) at airports, military, weather installations
Side Looking Radar
Synthetic Aperture Radar
Burst of single wavelength with echo/backscatter recorded
length of time for signal to return determines distance
strength of returning signal indicates composition
Some terms to know:
depression angle (angle of signal from horizontal)
look angle (angle of signal from nadir)
Applications
Penetration of smoke, canopy, clouds, snow
Creation of DEMs using interferometric radar
Estimates of moisture content with passive microwave
Detection of vertically/horizontally aligned objects (e.g., trees, downed wood, rail road tracks, power lines) with polarized radar
and more, limited only by one's imagination
Controls on Radar Return Signal
Surface Roughness relative to Wave Length
roughness elements < (wavelength/~25), then specular
(wavelength/25) < roughness element size < (wavelength/4.4), then intermediate
roughness > (wavelength/4.4), then diffuse
or in other words, smooth surfaces more mirror like, rough surfaces more diffuse
Depression angle
steeper depression angle = stronger return
Geometry of object
corner reflectors = very bright return
Electrical characteristics of object
greater conductivity = greater reflectance
water and metal are highly conductive
Topography
shadows
layover effects
Spatial Resolution
Across Track or Range Resolution
Resolution improves with decreasing depression angle (i.e., with increasing distance from aircraft)
Along Track or Azimuth Resolution
Resolution improves with increasing depression angle (i.e., closer to aircraft)
Concept of Polarization
Signals (HH, VV, HV, VH)
Generally used to detect object oriented in same way as signal
e.g., VV good for trees poles
e.g., HH good for downed wood, roads, railroads
VIII. Lidar (light detection and ranging)
Basic concept
Coherent vs. normal light
How laser profile is created
small and large footprint lidar
Multiple returns and different layers
First (primary); secondary and last returns (partial returns)
Bare earth DEM
Canopy mappig
Postings and interpolation to generate DEM
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