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Introduction to Remote Sensing Introduction to Remote Sensing Example Applications and Principles Exploring Images with Exploring Images with MultiSpec MultiSpec User Interface and Band Combinations Questions… Questions…

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Introduction to Remote Sensing Example Applications and Principles Exploring Images with MultiSpec User Interface and Band Combinations Questions…. Definitions. - PowerPoint PPT Presentation

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Page 1: Introduction to Remote Sensing  Example Applications and Principles

Introduction to Remote SensingIntroduction to Remote Sensing Example Applications and Principles

Exploring Images with MultiSpecExploring Images with MultiSpec User Interface and Band Combinations

Questions…Questions…

Page 2: Introduction to Remote Sensing  Example Applications and Principles

DefinitionsDefinitions

Lillesand and Kiefer (1994)Lillesand and Kiefer (1994) – ““The science and art The science and art of obtaining information …acquired by a of obtaining information …acquired by a device that is not in contact with the device that is not in contact with the object…object…””

CCRS GlossaryCCRS Glossary – “A group of techniques for A group of techniques for collecting image or other forms of datacollecting image or other forms of data … … from measurements made at a distance from measurements made at a distance from the object, from the object, and the processing and and the processing and analysis of the dataanalysis of the data.”.”

Page 3: Introduction to Remote Sensing  Example Applications and Principles

Examples of Remotely Sensed DataExamples of Remotely Sensed Data

Weather Ocean Properties Physical Geography Major Disturbance Events / Hazards Cultural Features – urban mapping Many other examples – thematic info

Page 4: Introduction to Remote Sensing  Example Applications and Principles
Page 5: Introduction to Remote Sensing  Example Applications and Principles

back

Page 6: Introduction to Remote Sensing  Example Applications and Principles

back

disturbance

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back

Page 8: Introduction to Remote Sensing  Example Applications and Principles

back

Page 9: Introduction to Remote Sensing  Example Applications and Principles
Page 10: Introduction to Remote Sensing  Example Applications and Principles

From Lillesand and Kiefer (1994)

Decision

Page 11: Introduction to Remote Sensing  Example Applications and Principles

Decision

From Lillesand and Kiefer (1994)

Page 12: Introduction to Remote Sensing  Example Applications and Principles
Page 13: Introduction to Remote Sensing  Example Applications and Principles

From Lillesand Kiefer (1994)

An Electromagnetic Wave

ll = wavelength = wavelength

nn = frequency = frequencyc = velocity of lightc = velocity of light

Page 14: Introduction to Remote Sensing  Example Applications and Principles
Page 15: Introduction to Remote Sensing  Example Applications and Principles
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OO33 absorption absorption at 0.2 at 0.2 uumm

Page 19: Introduction to Remote Sensing  Example Applications and Principles

HH22O absorption O absorption at 1.4, 1.6, and 1.9 at 1.4, 1.6, and 1.9 uumm

Page 20: Introduction to Remote Sensing  Example Applications and Principles

COCO22 absorption absorption at 2.0 at 2.0 uumm

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CHCH44 absorption absorption at 2.2 – 2.5 at 2.2 – 2.5 uumm

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Human eyeHuman eye

Page 23: Introduction to Remote Sensing  Example Applications and Principles

Incident EnergyIncident Energy Reflected EnergyReflected Energy

E(E(ll))ii – [ E( – [ E(ll))aa + E( + E(ll))t t ] = E] = Err((l)l)

Page 24: Introduction to Remote Sensing  Example Applications and Principles

Rayleigh ScatteringRayleigh Scattering

Rayleigh Scattering as a Function of Wavelength

0

5

10

15

20

25

30

35

40

45

0.4 0.45 0.5 0.55 0.6 0.65 0.7 0.75 0.8

Micrometers (um)

Rel

ativ

e In

ten

sity

of

Sca

tter

ing

Atmospheric InteractionsAtmospheric Interactions

Page 25: Introduction to Remote Sensing  Example Applications and Principles

Types of Satellite OrbitsTypes of Satellite Orbits

Geostationary – 35,790 km above the EarthGeostationary – 35,790 km above the Earth

Sun-synchronous or “Polar”– between 700 and 800 Sun-synchronous or “Polar”– between 700 and 800 km above the Earthkm above the Earth

Page 26: Introduction to Remote Sensing  Example Applications and Principles

Satellite Orbits

http://science.nasa.gov/Realtime/jtrack/3d/JTrack3D.htmlhttp://science.nasa.gov/Realtime/jtrack/3d/JTrack3D.html

Page 27: Introduction to Remote Sensing  Example Applications and Principles
Page 28: Introduction to Remote Sensing  Example Applications and Principles

““Resolution” in Remote SensingResolution” in Remote Sensing

Four typesFour types

1)1) SpatialSpatial –the ground coverage / pixel –the ground coverage / pixel

2) 2) SpectralSpectral – area and subdivision of the EM spectrum – area and subdivision of the EM spectrum

3) 3) TemporalTemporal – frequency of coverage – frequency of coverage

4)4) RadiometricRadiometric – sensitivity to changes in energy intensity – sensitivity to changes in energy intensity

Page 29: Introduction to Remote Sensing  Example Applications and Principles

Issues of spatial & temporal scale Issues of spatial & temporal scale of the sensor platformof the sensor platform

--SPATIAL-SPATIAL-

““grain” and “extent”grain” and “extent”

‘‘Pixel’Pixel’

-TEMPORAL--TEMPORAL-

Frequency of imagingFrequency of imaging

Page 30: Introduction to Remote Sensing  Example Applications and Principles
Page 31: Introduction to Remote Sensing  Example Applications and Principles

September 15September 15 September 30September 30

October 15October 15 October 30October 30

Page 32: Introduction to Remote Sensing  Example Applications and Principles

Color Theory and Band CombinationsColor Theory and Band Combinations

AdditiveAdditive colors vs. colors vs. SubtractiveSubtractive colors colors

‘‘Natural’ and ‘False’ color compositesNatural’ and ‘False’ color composites

Displaying images, extracting informationDisplaying images, extracting information

Page 33: Introduction to Remote Sensing  Example Applications and Principles

Additive PrimariesAdditive Primaries

Subtractive PrimariesSubtractive Primaries

No single primary can be formed by No single primary can be formed by mixture of other twomixture of other two

All other colors can be formed by All other colors can be formed by mixtures of additivesmixtures of additives

Representations of color via Representations of color via pigments and dyespigments and dyes

Yellow absorbs blue, cyan absorbs Yellow absorbs blue, cyan absorbs red, magenta absorbs greenred, magenta absorbs green

Page 34: Introduction to Remote Sensing  Example Applications and Principles

Blue (0.45 um) Green (0.55 um) Red (0.65 um)

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Blue (0.45 um) Green (0.55 um) Red (0.65 um)

Green = 2.5 x

Red = x Blue = x

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Feb. 14, 2006 MODIS Terra, Eastern US

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Snow Vs. Clouds

Clouds scatterat all wavelengths

Snow absorbs at >1.4 m

Page 38: Introduction to Remote Sensing  Example Applications and Principles

Snow Vs. Clouds

Clouds scatterat all wavelengths

Snow absorbs at >1.4 m

c

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Natural Color Natural Color 33,,22,1,1

Color IR Color IR 44,,33,2,2

False Color False Color 55,,44,3,3

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MultiSpec RS SoftwareMultiSpec RS Software

Research and educationResearch and education Long period development and refinementLong period development and refinement Freely availableFreely available Supported by tutorialsSupported by tutorials

http://cobweb.ecn.purdue.edu/~biehl/MultiSpec/http://cobweb.ecn.purdue.edu/~biehl/MultiSpec/