Chapter 1 Flashcards

λ wavelength f/v frequency μm micrometer 10^-6 nm 10^-9 Ang 10^-10 

1
Q
  • Define Remote Sensing
A

Collection of information about an object or system without coming into direct physical contact with it. That information is nearly always carried by electromagnetic radiation (EMR).

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2
Q

What sort of measurements in Remote Sensing (laundry list)

A

Measuring force fields, EMR, or acoustic energy employing cameras, radiometers and scanners, lasers, radio frequency receivers, radar systems, sonar, thermal devices, seismographs, magnetometers, gravimeters, scintillometers, and other instruments

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3
Q

Seven reasons we do remote sensing?

A

Unobtrusive.
Automated.
Useful for extreme conditions.
Combination of spatial and temporal coverage.
Extends our senses (beyond visible light)
Near real-time
No political boundary?

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4
Q

Spatial coverage

A

Global, regional, local

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5
Q

Seven Applications of remote sensing

A
  • Meteorology
  • Oceanography
  • Glaciology Sea Ice Research
  • Geology
  • Agriculture
  • Hydrology
  • Disaster control
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6
Q

Meteorlogy uses of remote sensing

A

– Profiling atmospheric temperatures and water vapor
– Measuring wind speed
– Watching evolution and trajectories of storms

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7
Q

Oceanography uses of remote sensing

A

– Measuring sea surface temperatures and salinity – Mapping of ocean currents
– Measuring sea level rise and variability

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8
Q

Glaciology uses of remote sensing

A

– Mapping motion of glaciers and ice sheets
– Monitoring ice melt
– Determining navigability of polar oceans

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9
Q

Geology uses of remote sensing

A

– Identification of rock types

– Location of geological faults and anomalies

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10
Q

Agriculture uses of remote sensing

A

– Monitoring extent and type of vegetation
– Mapping soil types
– Estimating vegetation biomass

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11
Q

Hydrology uses of remote sensing

A

– Assessing water resources
– Forecasting melt water runoff from snow
– Determining soil moisture

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12
Q

Diaster control uses of remote sensing

A

– Warnings of sand and dust storms
– Flooding
– Monitoring of pollution

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13
Q

Analog benefits (4)

A
– Medium is film
Benefits
• Easy to view
• High spatial resolution
• Sometimes cost-effective 
• Compact
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14
Q

Analog drawbacks (4)

A

– Medium is film
Drawbacks
• Difficult to transmit remotely
• Difficult to edit after acquisition
• Limited response to light (visible and near infrared wavelengths only)
• Degradation over time can limit archive capabilities

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15
Q

Digital benefits (4)

A
• Wide variety of detectors
     – Electromagnetic and other types 
     – Large amplitude range
• Data easily transmitted remotely
• Data easily edited/manipulated/enhanced after acquisition 
• Long-term archive
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16
Q

Digital drawbacks (3)

A
  • Storage requirements can be large
  • Reduced spatial resolution in many cases
  • Requires sophisticated equipment and analysis techniques to use
17
Q

Four types of Remote Sensing Systems

A
  • Active Sensor – illuminates subject from an artificial (on- board) energy source
  • Passive sensor – uses naturally emitted radiation from the sun or the object being observed
  • Imaging sensor – creates a “picture” by scanning across a linear array of detectors while the array moves through space
  • Non-imaging sensors – measures along a transect or at a point
18
Q

5 characters for Summarizing Remote Sensing Systems

A
  • Platform:Ground,airborne,satellite
  • Media: digital or analog
  • Illumination: passive or active
  • Detector configuration: imaging, single-point, transect or sounding
  • Spectralrange:visible,infrared,microwave,etc.
19
Q

Conduction

A

transfer of kinetic energy between atoms or

molecules

20
Q

Convection

A

transfer of kinetic energy by physically moving mass that contains that energy

21
Q

Radiation

A

propagation via waves or particles through a vacuum or medium

22
Q

Sources of EMR (active and passive)

A

– Sun and Earth are both passive sources of EM radiation

– Lasers and radars are active sources of EM radiation

23
Q

How is EMR generated?

A

– Kinetic: motion of atoms or molecules producing heat (thermal)
– Electrical: generation of electric fields radio frequency
– Magnetic: polarization of charged atoms (microwave)
– Chemical: molecular excitation (visible)

24
Q

Electromagnetic waves (basic definition)

A

Energy travels in waves described by
– Wavelength λ ( of frequency f/v), crest to crest
– Amplitude (a), crest to midline

25
Q

Visible wavelength range

A

λ = 390 nm – 750 nm (3.9 - 7.5 x10^-7 m)
Blue:.4-.5 μm
Green: .5-.6 μm
Red: .6 - .7 μm

26
Q

Most common remote sensing data types (EMR)

A

visible, infrared, thermal, and microwave

• Sun (most impt)
– Reflected solar energy 0.3 – 2.5 (3) μm
• Earth
– > 6 μm for self-emitted energy

μm = 1x 10^-6 m

27
Q

Applications for Remote sensing (Summary)

A

• Remotely gathering information carried by EMR
• Quantitative analysis of digital information
– Image interpretation from hard copy is history
– Additional computational and analytical skills are required
• Global change issues can be addressed
• Highly interdisciplinary

28
Q

Microwave wavelength range

A

λ = 1 mm – 1 m ( 1 x 10^-7 to 1 x 10^-9 nm))

29
Q

Infrared wavelength range

A

λ = .75 - 30 μm (1,000 nm – 30,000 nm)

near IR = .75 to 1.3 μm
mid (short-wave) = 1.3 - 3 μm
thermal IR = two bands 3 - 5 μm and 8-14 μm
far IR = 3 - 30 μm

30
Q

Collateral data

A

Aka ancillary data

Digital elevation models (DEMs), maps, political boundary files, population stats, etc. often in GIS

30
Q

Formula for relationship between wavelength and freq

A

c = λv

3.0 x 10^8 m/s = λ (in μm or nm) x v (in Hz, or 1/s)

31
Q

Add spectral ranges

A

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