Study Guide for First Midterm
Geography 418/518, Fundamentals of Remote Sensing
Winter, 2007
Note: materials below are guide to what was covered in lectures and text book. You must also review materials on web-based readings, which are not included in review list below.
NOTE: Andrew will be available on Tuesday, Feb 13 from 11-noon in his office if you have questions)
The first midterm covers lectures through week 5 (through geometric corrections), the labs through week 4 (general process questions, not which software command to use questions), and the following readings: 3rd edition - 1, 2, 4, 6 (skim) 9 and 10.5-10.6; 4th edition: Chap 1,2,4, 6 (skim), 10 and 11.5-11.6.
As you study for the midterm, you should focus first on lecture notes and the text book - the majority of questions come from these sources. Pay particular attention to diagrams in the book and online readings. You should understand and be able to explain the concepts presented in the labs (how data are stored as numbers, how different bands can be displayed in "false" colors, the nature of raster data). Do not worry, however, about remembering details about the software (e.g., different ways to zoom in on the image). Finally, do complete the on-line readings. I may have questions from the on-line NASA tutorials on the test. Remember that I have not summarized the on-line materials below in the study guide - you will have to do this yourself.
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. Introduction to Remote Sensing
Definition of R.S.
Potential advantages/disadvantages of using R.S.
Speed
Document processes/features that cannot be detected otherwise
Cost
Accuracy
Permanent record
Reproducible record
Analytical capability (quantitative analysis)
Decision to use or not to use R.S. dependent on:
What you want to detect
When you want to detect it
Where you want to see it
Logistical constraints
II Brief History of Remote Sensing (see on-linereadings)
Early developments
~350 B.C., Aristotle and camera obscura
1839, Daguerre an Niepce create the Daguerrotype
1903, the Wright brothers and first airplane
Importance of World War I and World War II
Technological advances
Training of large numbers of photo interpreters
Development of rockets
The Space Age
Development of new platforms (rockets and satellites)
Development of new sensors (digital and multispectral)
Development of computers
Still a very young and developing science
III The Remote Sensing System
Energy Sources
passive
active
the electromagnetic spectrum
Energy Movement through the Atmosphere and at the Earth's Surface
Absorption
Scattering
Reflection
Transmission
Fluorescence (in the book)
Sensor Systems and Platforms
Data Handling Systems
Data User
IV. The Electromagnetic Spectrum
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
Radiation laws (general concepts, not the equations)
Wien's Law
Stefan-Boltzman Law
Concept and application of additive colors (e.g., how we generate the colors we see on a computer screen with mixtures of red, blue, green).
V. Energy Interactions in the Atmosphere
Scattering ( for the scattering types below be able to describe which wavelengths are affected and how to avoid that type of scattering)
Rayleigh
role in controlling sky color and sunsets
how this can affect contrast on a clear day image
Mie
Nonselective
Absorption
Atmospheric windows
Key gases controlling absorption
Transmission
Reflectance
specular
intermediate
diffuse
how variations in reflectance allow us to distinguish different features
VI. Multispectral Sensing Systems
Framing Systems (classic cameras)
Concept
Advantages (similar to human eye, easier to interpret)
Disadvantages (multiples lens, tough to register, historically film-based and not digital)
Analog to Digital Systems (A to D)
Concept: multispectral scanner with cross track scanning (whisk broom)
Advantages (wide field of view, broad spatial coverage, more frequent coverage, one sensor per band)
Disadvantages
short dwell time
historically a lower spectral resolution
more geometric distortion
tangential-scale distortion
resolution cell size variations
one dimensional relief displacement
flight parameter distortions
Charge Coupled Device (CCD) Systems
Concept: multispectral scanner with along track (push broom) scanning
Advantages (longer dwell time, historically better spatial resolution and higher spectral resolution, less geometric distortion)
Disadvantages (less spatial coverage, more sensors and calibration issues, less frequent coverage, unable to cover wavelengths longer than mid-IR)
Resolution
Spatial (the ability to resolve objects of a given size)
Controls
target variables (contrast, shape, size, spacing, number, background uniformity)
system variables (IFOV, scan speed, instrumentation)
operating conditions (atmospheric scattering, absorption)
Advantages of fine spatial resolution (more spatial detail)
Disadvantages of fine spatial resolution relative to coarse resolution imagery (assuming same image "footprint")
more data storage required
shorter dwell time leads to
weaker signal per pixel
lower spectral resolution
finer resolution images cover a smaller area
because a smaller area is covered, the return interval to get to that area is much longer (assuming satellite imagery) - i.e., poorer frequency of coverage
Temporal (repeat interval)
Controls
Velocity of platform
Image footprint (i.e., area covered in one image)
Advantages of more frequent coverage
ability to avoid cloud cover
closer to real time monitoring
Disadvantages of more frequent coverage
usually required greater footprint, which means coarser resolution
Spectral (the ability to detect variations within a given bandwidth)
Controls
dwell time (longer dwell = more energy = more ability to resolve spectra)
spatial resolution (bigger area = more energy = better resolving capability)
image brightness
instrumentation (signal to noise ratio)
Advantages of finer spectral resolution - enhances ability to differential objects with small variations in spectral signal
Disadvantage: more data storage if many narrow spectral ranges (i.e. hyperspectral)
Radiometric (in multispectral system, the smallest variation in reflectance that is recorded)
Largely controlled by signal to noise ratio
Advantage of finer radiometric resolution: ability to detect subtle differences between objects
Disadvantage: finer resolution requires more data storage
Landsat, SPOT. IKONOS, AVHRR (examples of the concepts above - see Chapter 6)
Orbits and rationale
near polar
sun synchronous
crossover timing and rationale
Systems
Relative spatial resolutions:
Relative temporal resolutions
Relative spectral resolutions
VII. 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
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