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Some Basic Concepts of
Remote Sensing
Remote sensing platformsRemote sensing platforms
Ground-based Airplane-based Satellite-based
Satellite Based
 Sun-synchronous polar orbits
 Most earth imaging satellites is polar-orbiting, meaning that they circle the
planet in a roughly north-south ellipse while the earth revolves beneath them.
Therefore, unless the satellite has some sort of "pointing" capability, there are
only certain times when a particular place on the ground will be imaged
 global coverage, fixed crossing, repeat sampling
 typical altitude 500-1,500 km
 example: Terra/Aqua, Landsat
 Non-Sun-synchronous orbits
 Tropics, mid-latitudes, or high latitude coverage, varying sampling
 typical altitude 200-2,000 km
 example: TRMM, ICESat
 Geostationary orbits
 regional coverage, continuous sampling
 over low-middle latitudes, altitude 35,000 km
 example: GOES. http://www.nesdis.noaa.gov/SatInformation.html
Types of remote sensing
 Passive: source of
energy is either the Sun
or Earth/atmosphere
 Sun
- wavelengths: 0.4-5
µm
 Earth or its atmosphere
- wavelengths: 3 µm
-30 cm
 Active: source of
energy is part of the
remote sensor system
 Radar
- wavelengths: mm-m
 Lidar
- wavelengths: UV,
Visible, and near
infrared
Camera takes photo as example, no flash and flash
elevation angle ( α) = 90-θ, some time, elevation angle is also called altitude
αs
αv
Solar incidence angle is the angle between the Sun and a line perpendicular to a surface. So
solar zenith angle is the solar incidence angle for a horizontal surface. For a slope surface,
they are different.
Azimuth angle definition difference: starts from north or from south:
http://www.serd.ait.ac.th/ep/mtec/selfstudy/Chapter1/position.html
Four types of resolution
 Spatial resolution
 Spectral resolution
 Radiometric resolution
 Temporal resolution
Spatial resolution and coverage
 Spatial resolution
 Instantaneous field-of-view
(IFOV)
 Pixel: smallest unit of an
image
 Pixel size
 Spatial coverage
 Field of view (FOV), or
 Area of coverage, such as
MODIS: 2300km or global
coverage, weather radar
(NEXRAD): a circle with
230 km as radius
30 meter, spatial resolution
Northwest San Antonio
1 meter, spatial resolution
UTSA campus,
red polygon is the Science Building
SpatialSpatial
ResolutionResolution
SpatialSpatial
ResolutionResolution
Jensen, 2000
Jensen, 2000
Spectral resolution (∆λ ) and
coverage (λmin to λmax)
 Spectral resolution
describes the ability of
a sensor to define fine
wavelength intervals
 The finer the spectral
resolution, the
narrower the
wavelength range for a
particular channel or
band
Radiometric resolution and coverage
 Sensor’s sensitivity to the magnitude of the
electromagnetic energy,
 Sensor’s ability to discriminate very slight
differences in (reflected or emitted) energy,
 The finer the radiometric resolution of a sensor,
the more sensitive it is to detecting small
differences in energy
Comparing a 2-bit image with an 8-bit image
Basics of Bit
 Computer store
everything in 0 or 1
bits Max. num
1 2
2 4
3 8
6 64
8 256
11 2048
12 4096
(2bits
)
7 6 5 4 3 2 1 0
0 0 0 0 0 0 0 0
1 1 1 1 1 1 1 1
Bit no.
0
256
8 bits as an example Resolution: 12 bits
Coverage: 0 - 4095
Temporal resolution and coverage
 Temporal resolution is the revisit period, and is the
length of time for a satellite to complete one entire
orbit cycle, i.e. start and back to the exact same area
at the same viewing angle. For example, Landsat
needs 16 days, MODIS needs one day, NEXRAD
needs 6 minutes for rain mode and 10 minutes for
clear sky mode.
 Temporal coverage is the time period of sensor from
starting to ending. For example,
 MODIS/Terra: 2/24/2000 through present
 Landsat 5: 1/3/1984 through present
 ICESat: 2/20/2003 to 10/11/2009
Remote Sensing Raster (Matrix) Data FormatRemote Sensing Raster (Matrix) Data FormatRemote Sensing Raster (Matrix) Data FormatRemote Sensing Raster (Matrix) Data Format
0
127
255
Brightnessvalue
range
(typically8bit)
Associated
gray-scale
10 15 17 20
15 16 18 21
17 18
20
22
18
20
22 24
1
2
3
4
1 5432
Columns (j)
Bands (k)
1
2
3
4
Xaxis Pictureelement(pixel)atlocation
Line4,Column4,inBand1hasa
BrightnessValueof24,i.e.,BV4,4,1 =24.
black
gray
white
21
23
22
25
Linesor
rows(i)
0
127
255
Brightnessvalue
range
(typically8bit)
Associated
gray-scale
10 15 17 20
15 16 18 21
17 18
20
22
18
20
22 24
1
2
3
4
1 5432
Columns (j)
Bands (k)
1
2
3
4
Xaxis Pictureelement(pixel)atlocation
Line4,Column4,inBand1hasa
BrightnessValueof24,i.e.,BV4,4,1 =24.
black
gray
white
21
23
22
25
Linesor
rows(i)
Jensen, 2000Jensen, 2000Jensen, 2000Jensen, 2000
Y
axis
Field of View (FOV), Instantaneous Field of View (IFOV)
Dwell time is the time required for the detector IFOV to sweep across a ground cell. The longer
dwell time allows more energy to impinge on the detector, which creates a stronger signal.
Sabin, 1997
Wiskbroom
Pushbroom
Remote
Sensing
Scanning
System
IFOV and FOV
IFOV= 2 tag-1
(d / 2f) ≈ d / f (radians). (d is the detector size, f is the focal
length). The general unit of IFOV is milliradians (10-3
radians).
1º = (2π/360) = 0.01745 radians = 17.45 milliradians
1 milliradian = 0.057 º
lens
FOV= 2 tag-1
(D / 2f) (degree)
Detector
configurations:
breaking up the
spectrum
 Discrete Detectors and scanning
mirrors
- MSS, TM, ETM+, GOES, AVHRR,
SeaWiFS, AMS, ATLAS
 Linear Arrays
- SPOT, IRS, IKONOS,
ORBIMAGE, Quickbird, ASTER,
MISR
 Liner and area arrays
- AVIRIS, CASI, MODIS, ALI,
Hyperion, LAC
Slides for your references
only
Ustin, 2003
Ustin, 2003
Ustin, 2003
Ustin, 2003
Ustin, 2003
Ustin, 2003

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Rs

  • 1. Some Basic Concepts of Remote Sensing
  • 2. Remote sensing platformsRemote sensing platforms Ground-based Airplane-based Satellite-based
  • 3. Satellite Based  Sun-synchronous polar orbits  Most earth imaging satellites is polar-orbiting, meaning that they circle the planet in a roughly north-south ellipse while the earth revolves beneath them. Therefore, unless the satellite has some sort of "pointing" capability, there are only certain times when a particular place on the ground will be imaged  global coverage, fixed crossing, repeat sampling  typical altitude 500-1,500 km  example: Terra/Aqua, Landsat  Non-Sun-synchronous orbits  Tropics, mid-latitudes, or high latitude coverage, varying sampling  typical altitude 200-2,000 km  example: TRMM, ICESat  Geostationary orbits  regional coverage, continuous sampling  over low-middle latitudes, altitude 35,000 km  example: GOES. http://www.nesdis.noaa.gov/SatInformation.html
  • 4. Types of remote sensing  Passive: source of energy is either the Sun or Earth/atmosphere  Sun - wavelengths: 0.4-5 µm  Earth or its atmosphere - wavelengths: 3 µm -30 cm  Active: source of energy is part of the remote sensor system  Radar - wavelengths: mm-m  Lidar - wavelengths: UV, Visible, and near infrared Camera takes photo as example, no flash and flash
  • 5. elevation angle ( α) = 90-θ, some time, elevation angle is also called altitude αs αv
  • 6. Solar incidence angle is the angle between the Sun and a line perpendicular to a surface. So solar zenith angle is the solar incidence angle for a horizontal surface. For a slope surface, they are different. Azimuth angle definition difference: starts from north or from south: http://www.serd.ait.ac.th/ep/mtec/selfstudy/Chapter1/position.html
  • 7. Four types of resolution  Spatial resolution  Spectral resolution  Radiometric resolution  Temporal resolution
  • 8. Spatial resolution and coverage  Spatial resolution  Instantaneous field-of-view (IFOV)  Pixel: smallest unit of an image  Pixel size  Spatial coverage  Field of view (FOV), or  Area of coverage, such as MODIS: 2300km or global coverage, weather radar (NEXRAD): a circle with 230 km as radius
  • 9. 30 meter, spatial resolution Northwest San Antonio 1 meter, spatial resolution UTSA campus, red polygon is the Science Building
  • 11. Spectral resolution (∆λ ) and coverage (λmin to λmax)  Spectral resolution describes the ability of a sensor to define fine wavelength intervals  The finer the spectral resolution, the narrower the wavelength range for a particular channel or band
  • 12. Radiometric resolution and coverage  Sensor’s sensitivity to the magnitude of the electromagnetic energy,  Sensor’s ability to discriminate very slight differences in (reflected or emitted) energy,  The finer the radiometric resolution of a sensor, the more sensitive it is to detecting small differences in energy
  • 13. Comparing a 2-bit image with an 8-bit image
  • 14. Basics of Bit  Computer store everything in 0 or 1 bits Max. num 1 2 2 4 3 8 6 64 8 256 11 2048 12 4096 (2bits ) 7 6 5 4 3 2 1 0 0 0 0 0 0 0 0 0 1 1 1 1 1 1 1 1 Bit no. 0 256 8 bits as an example Resolution: 12 bits Coverage: 0 - 4095
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  • 16. Temporal resolution and coverage  Temporal resolution is the revisit period, and is the length of time for a satellite to complete one entire orbit cycle, i.e. start and back to the exact same area at the same viewing angle. For example, Landsat needs 16 days, MODIS needs one day, NEXRAD needs 6 minutes for rain mode and 10 minutes for clear sky mode.  Temporal coverage is the time period of sensor from starting to ending. For example,  MODIS/Terra: 2/24/2000 through present  Landsat 5: 1/3/1984 through present  ICESat: 2/20/2003 to 10/11/2009
  • 17. Remote Sensing Raster (Matrix) Data FormatRemote Sensing Raster (Matrix) Data FormatRemote Sensing Raster (Matrix) Data FormatRemote Sensing Raster (Matrix) Data Format 0 127 255 Brightnessvalue range (typically8bit) Associated gray-scale 10 15 17 20 15 16 18 21 17 18 20 22 18 20 22 24 1 2 3 4 1 5432 Columns (j) Bands (k) 1 2 3 4 Xaxis Pictureelement(pixel)atlocation Line4,Column4,inBand1hasa BrightnessValueof24,i.e.,BV4,4,1 =24. black gray white 21 23 22 25 Linesor rows(i) 0 127 255 Brightnessvalue range (typically8bit) Associated gray-scale 10 15 17 20 15 16 18 21 17 18 20 22 18 20 22 24 1 2 3 4 1 5432 Columns (j) Bands (k) 1 2 3 4 Xaxis Pictureelement(pixel)atlocation Line4,Column4,inBand1hasa BrightnessValueof24,i.e.,BV4,4,1 =24. black gray white 21 23 22 25 Linesor rows(i) Jensen, 2000Jensen, 2000Jensen, 2000Jensen, 2000 Y axis
  • 18. Field of View (FOV), Instantaneous Field of View (IFOV) Dwell time is the time required for the detector IFOV to sweep across a ground cell. The longer dwell time allows more energy to impinge on the detector, which creates a stronger signal. Sabin, 1997 Wiskbroom Pushbroom Remote Sensing Scanning System
  • 19. IFOV and FOV IFOV= 2 tag-1 (d / 2f) ≈ d / f (radians). (d is the detector size, f is the focal length). The general unit of IFOV is milliradians (10-3 radians). 1º = (2π/360) = 0.01745 radians = 17.45 milliradians 1 milliradian = 0.057 º lens FOV= 2 tag-1 (D / 2f) (degree)
  • 20. Detector configurations: breaking up the spectrum  Discrete Detectors and scanning mirrors - MSS, TM, ETM+, GOES, AVHRR, SeaWiFS, AMS, ATLAS  Linear Arrays - SPOT, IRS, IKONOS, ORBIMAGE, Quickbird, ASTER, MISR  Liner and area arrays - AVIRIS, CASI, MODIS, ALI, Hyperion, LAC
  • 21. Slides for your references only

Hinweis der Redaktion

  1. launch 1972, Landsat MSS, TM, ETM+ 1999, NASA flagship satellite “Terra” with 5 state-of-the-art sensors for studying the Earth’s atmosphere, land, ocean, life, and radiation 1999, the first high-resolution commercial satellite IKONOS