3. Remote Sensing Defined
Remote Sensing is:
“The art and science of obtaining information
about an object without being in direct contact
with the object” (Jensen 2000).
There is a medium of transmission involved.
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
4. ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
5. Remote Sensing Defined
Environmental Remote Sensing:
… the collection of information about Earth surfaces
and phenomena using sensors not in physical contact
with the surfaces and phenomena of interest.
We will focus on data collected from an overhead
perspective via transmission of electromagnetic
radiation.
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
7. Remote Sensing Defined
Remote Sensing Includes:
A) The mission plan and choice of sensors;
B) The reception, recording, and processing of the
signal data; and
C) The analysis of the resultant data.
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
8. Types of Remote Sensing:Sensing:Based on Range of Electromagnetic
Spectrum:Spectrum:1. Optical Remote Sensing.
2. Thermal Remote Sensing.
3.
Microwave Remote Sensing.
Based on the source of the energy:energy:Active remote sensing.
Passive remote sensing.
1.
2.
9. Based on Range of Electro
magnetic Spectrum:Spectrum:
Optical Remote Sensing:Sensing:The optical remote sensing devices
operate in the visible, near infrared,
middle infrared and short wave
infrared portion of the electromagnetic
spectrum.
These devices are sensitive to the
wavelengths ranging from 300 nm to
3000 nm.
10. Thermal Remote Sensing:Sensing:
The sensors, which operate in
thermal range of electromagnetic
spectrum record, the energy
emitted from the earth features in
the wavelength range of 3000 nm to
5000 nm and 8000 nm to 14000 nm.
11. Microwave Remote Sensing:Sensing:
A microwave remote sensor records the
backscattered microwaves in the
wavelength range of 1 mm to 1 m of
electromagnetic spectrum.
Most of the microwave sensors are active
sensors, having there own sources of
energy.
12. Depending on the source of the
energy:energy:
Active remote sensing:sensing:Active remote sensing uses an artificial source for
energy.
For example the satellite itself can send a pulse of
energy which can interact with the target.
In active remote sensing, humans can control the
nature (wavelength, power, duration) of the source
energy.
Active remote sensing can be carried out during
day and night and in all weather conditions.
ExampleExample- RADAR
13. Passive remote sensing:sensing:
Passive remote sensing depends on a natural
source to provide energy.
The sun is the most powerful and commonly
used source of energy for passive remote
sensing.
The satellite sensor in this case records primarily
the radiation that is reflected from the target.
15. Remote Sensing Process Components
Energy Source or Illumination (A)
Radiation and the Atmosphere (B)
Interaction with the Target (C)
Recording of Energy by the Sensor (D)
Transmission, Reception, and
Processing (E)
Interpretation and Analysis (F)
Source: Canadian Centre for Remote Sensing
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
Application (G)
17. Advantages of remote sensing:sensing:
Provides a regional view (large areas).
Provides repetitive looks at the same area.
Remote sensors "see" over a broader.
portion of the spectrum than the human
eye.
Provides geo-referenced, digital, data.
geoSome remote sensors operate in all
seasons, at night, and in bad weather.
Give information of inaccessible area.
18. DISADVANTAGE OF REMOTE
SENSING:SENSING:• Expensive to build and operate.
• Measurement uncertainty can be
large.
• Data interpretation can be difficult.
19. Applications of Remote
Sensing:Sensing:
Agriculture:Agriculture:Crop type classification.
Crop condition assessment.
Crop yield estimation.
Mapping of soil characteristic.
Soil moisture estimation.
25. Resolution
All remote sensing systems have four types of
resolution:
Spatial
Spectral
Temporal
Radiometric
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
26. Spatial Resolution
High vs. Low?
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
Source: Jensen (2000)
28. Temporal Resolution
July 2
July 18
August 3
16 days
Time
11 days
July 1
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
July 12
July 23
August 3
39. IKONOS (4 m Multispectral)
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
40. IKONOS (1 m Panchromatic)
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
41. RADAR
(Radio Detection and Ranging)
Image: NASA 2005
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
42. LIDAR
(Light Detection and Ranging)
Image: Bainbridge Island,
WA courtesy Pudget Sound
LIDAR Consortium, 2005
43. Elements of Image Interpretation
Shape:
Many natural and human-made features have
humanunique shapes.
Often used are adjectives like linear,
curvilinear, circular, elliptical, radial, square,
rectangular, triangular, hexagonal, star,
elongated, and amorphous.
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
45. Elements of Image Interpretation
Shadow:
Shadow reduction is of concern in remote sensing
because shadows tend to obscure objects that
might otherwise be detected.
However, the shadow cast by an object may be
the only real clue to its identity.
Shadows can also provide information on the
height of an object either qualitatively or
quantitatively.
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
47. Elements of Image Interpretation
Tone and Color:
A band of EMR recorded by a remote sensing
instrument can be displayed on an image in
shades of gray ranging from black to white.
These shades are called “tones”, and can be
qualitatively referred to as dark, light, or
intermediate (humans can see 40-50 tones).
40-
Tone is related to the amount of light reflected
from the scene in a specific wavelength interval
(band).
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
48. Tone and Color
Jensen (2000)
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
49. Elements of Image Interpretation
Texture:
Texture refers to the arrangement of tone or color
in an image.
Useful because Earth features that exhibit similar
tones often exhibit different textures.
Adjectives include smooth (uniform,
homogeneous), intermediate, and rough (coarse,
heterogeneous).
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
51. Elements of Image Interpretation
Pattern:
Pattern is the spatial arrangement of objects on
the landscape.
General descriptions include random and
systematic; natural and human-made.
human-
More specific descriptions include circular, oval,
curvilinear, linear, radiating, rectangular, etc.
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
53. Elements of Image Interpretation
Height and Depth:
As discussed, shadows can often offer clues to the
height of objects.
In turn, relative heights can be used to interpret
objects.
In a similar fashion, relative depths can often be
interpreted.
Descriptions include tall, intermediate, and short;
deep, intermediate, and shallow.
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
55. Elements of Image Interpretation
Association:
This is very important when trying to
interpret an object or activity.
Association refers to the fact that certain
features and activities are almost always
related to the presence of certain other
features and activities.
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
57. Digital Image processing
1.
2.
3.
Correction of data
Digital enhancement for the purpose of better visual
interpretation.
It involves three basic steps:
Image preprocessing
Image processing
Post processing & transformation
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
58. Why do we need image
processing?
o
o
o
Improvement of pictorial information for
human perception
Image processing for autonomous
machine application
Efficient storage and transmission
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
61. Geometric correction
Geometric corrections are made to correct the
inaccuracy between the location coordinates of the
picture elements in the image data, and the actual
location coordinates on the ground. Several types of
ground.
geometric corrections include system, precision, and
terrain corrections.
corrections.
62. Radiometric correction
Radiometric corrections are made to the raw digital
image data to correct for brightness values, of the object
on the ground, that have been distorted because of
sensor calibration or sensor malfunction problems. The
problems.
distortion of images is caused by the scattering of
reflected electromagnetic light energy due to a
constantly changing atmosphere. This is one source of
atmosphere.
sensor calibration error.
error.
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
63.
64. Image processing
Enhancing an image or extracting
information or features from an image
Computerized routines for information
extraction (eg, pattern recognition,
(eg,
classification) from remotely sensed
images to obtain categories of information
about specific features.
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
65.
Spatial filtering
Image quality and statistical evaluation
Image contrast enhancement and sharpening
Image classification
Pixel based
ObjectObject-oriented based
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005
66. Post processing & transformation
Accuracy assessment of classification
PostPost-classification and GIS
Change detection
ND GIS Users Workshop
Bismarck, ND October 24-26,
242005