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ERS186: Environmental Remote Sensing

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Title: ERS186: Environmental Remote Sensing


1
ERS186Environmental Remote Sensing
  • Lecture 1 Introduction

2
Welcome to ERS186!
  • Course instructors
  • Solomon Dobrowski szdobrowski_at_ucdavis.edu
  • Jonathan Greenberg greenberg_at_ucdavis.edu
  • Course website
  • http//www.cstars.ucdavis.edu/classes/ers186-w03
  • All lectures will be posted here, as well as any
    supplementary articles and relevant websites.
  • Course listserv
  • ers186-w03_at_ucdavis.edu
  • Please ask any general interest question here,
    but please dont send personal questions through
    this list!
  • Well occasionally send information through this
    listserv, so check your email!
  • Grading Midterm (40) and Final (60)
  • We will distribute practice questions before each
    exam a certain number of the practice questions
    will be WORD FOR WORD the same as the exam!
  • Office hours TR, 1200 to 100 location TBA

3
Text and Supplementary Info
  • Jensen, J. R. 2000. Remote Sensing of the
    Environment An Earth Resource Perspective.
    Prentice-Hall, Inc., Upper Saddle River, NJ.
  • Note this book (as far as we know) is also used
    in ERS185.
  • All other texts/articles will either be
    distributed in class or placed on the website.

4
Course Outline
  • Introduction (JG)
  • Principles of Electromagnetic Radiation (SD)
  • Remote sensing technology and terminology (JG)
  • Scaling up in remote sensing
  • Atoms and Molecules Geology (JG)
  • Microscopic particles Atmospheric Science,
    Climatology, Hydrology and Soil Science (SD)
  • Cells Agriculture and Ecology (SD) MIDTERM!
  • Plant structure Agriculture and Ecology (SD)
  • Mixed pixels Terrestrial and Aquatic Ecology
    Urban Landscapes (JG)
  • Field methodology and spatial analysis
  • Temporal image analysis and change detection (JG)
  • CSTARS lectures FINAL!

5
Course Goals
  • ERS186 to be able to read and evaluate remote
    sensing literature in the context of a
    mechanistic understanding of RS principles and
    technology.
  • Secondarily, you MUST know the difference between
    GPS, GIS and RS!
  • ERS186L (Spring) to be able to perform basic
    remote sensing research (project design, data
    collection, image acquisiton, image analysis,
    presentation of results).

6
What Is Remote Sensing?
  • From your text
  • Maximal definition (not very useful) remote
    sensing is the acquiring of data about an object
    without touching it.

7
What Is Remote Sensing?
  • From your text
  • Minimal definition (much better) remote sensing
    is the noncontact recording of information from
    the ultraviolet, visible, infrared, and microwave
    regions of the electromagnetic spectrum by means
    of instruments such as cameras, scanners, lasers,
    linear arrays, and/or area arrays located on
    platforms such as aircraft or spacecraft, and the
    analysis of acquired information by means of
    visual and digital image processing.

8
What Is Remote Sensing?
  • Some thoughts
  • We are NOT going to focus on visual
    interpretations, rather we will focus on digital
    technologies. Photogrammetry (visual/analog
    remote sensing) can be learned in ERS185.
  • Remote sensing is an applied science and is a
    tool to help understand other fields such as
    ecology, climatology, geology, soil science and
    hydrology.

9
What Is Not Remote Sensing?
GIS (Geographic Information Systems)
RS (Remote Sensing)
GPS (Global Positioning System)
10
A Whirlwind Tour Of RemoteSensing
11
Physics
12
Sensors and Technology
13
Geology Terrestrial
Nevada surface materials map based on specific
chemical bonds and AVIRIS hyperspectral
imagery. Analysis performed using Tetracorder
software (Trekkies feel free to laugh at this
name).
http//speclab.cr.usgs.gov/PAPERS/tetracorder/
14
Geology Planetary
Tharsis Volcanos on Mars Sensors MOLA and Viking
15
Atmospheric Science
Hurricane Dennis, GOES-9
16
Hydrology
Soil Equivalent Water Depth
Snow Depth
Surface Water Depth
Daily Transpiration
SPLASH hydrological data, LANDSAT inputs
17
Soil Science
18
Agriculture
Gallo Vineyards, Sonoma County, ADAR-5500
19
Ecology
Theodore Roosevelt National Park, North Dakota,
Leafy Spurge Mapping
20
Change Detection
Yasuni National Park, Ecuador, LANDSAT
21
Big Pictures
  • Much of the current remote sensing research is
    focusing on climate change and the carbon cycle.

22
Big Pictures
23
Hooray for Physics!!!
24
Electromagnetic Principles An overview of whats
to come.
  • Wave properties of light
  • Particle properties of light
  • Wave particle duality
  • Energy matter interactions
  • The remote sensing problem

25
Wave model of electromagnetic Radiation
26
How do we describe the wave?
Wavelength (?) the mean distance between
maximums (or minimums) of a periodic pattern.
Usually measured in nm (10-9 m) or ?m (10-6
m) Frequency (v) is the number of wavelengths
that pass a point per unit time. Measured in
hertz (Hz) or cycle per second. Speed of light
(c) 3x108 m/s in a vacuum
27
Wave equation (in a vacuum)
C ?v V c/ ? ? c/v
28
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29
Electromagnetic Spectrum
30
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31
The Speed of Light Revisited
In a vacuum C 3x108 m/s In material mediums the
velocity of the EMR depends on the frequency of
the wave but is never greater than C.
The index of refraction of the medium n
C/S Where S speed of light in a medium Note N
is always greater than 1
32
Wave Properties
Frequency of a light wave in a medium is
determined by its source and is unaffected by the
medium!!!
Thus, lets revisit the wave equation V ? S
C/N V ? C/N Which posits that the
wavelength changes when the index of refraction
changes
33
Wave Properties (continued)
When would the index of refraction change? when
light passes from one medium to another. In fact
? will decrease when moving from one medium to a
more optically dense medium. (extra credit?)
34
Wave Properties (continued)
Refraction When light goes from one transparent
medium to another with a different index of
refraction (N), the light is bent
Snells Law n1sin?1 n2sin?2 Where ? the
angle of incidence Note if n increases then
sin?, and consequently ? decreases
35
Wave Properties (continued)
36
Wave Properties (continued)
Since the index of refraction (n) of materials
varies with the wavelength of the light, the
amount of bending at boundaries will vary with
wavelength. This is known as dispersion and leads
to the separation of white light into colors by a
prism.
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