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Fundamentals of Remote
Sensing
Prof. Dr. Sajid Rashid Ahmad
sajidpu@yahoo.com
Atiqa Ijaz Khan _ Demonstrator
atiqa_ss09@yahoo.com
• What is Remote Sensing?
• If you are reading this sentence, now you are doing Remote Sensing. In fact, any
information acquired from the object without touching is Remote Sensing.
• Remote sensing offers the ability to observe and collect data for large areas relatively
quickly, and is an important source of data for GIS. (Source: digimap)
Monday, March 30, 2015Institute of Geology, University of the Punjab
2
Remote Sensing
• “The art and science of obtaining information about an object without
being in direct contact with the object” (Jensen 2000).
• The science (and art) of acquiring information about an object, without
entering in contact with it, by sensing and recording reflected or
emitted energy and processing, analyzing, and applying that
information.
• Information usually gathered from spacecraft or an airplane.
• In from of aerial photographs to satellite images.
Monday, March 30, 2015Institute of Geology, University of the Punjab
3
Monday, March 30, 2015Institute of Geology, University of the Punjab
4
Eyes
Binoculars Digital Camera
Pigeon Cameras
1903
Monday, March 30, 2015Institute of Geology, University of the Punjab
5Types
Terrestrial RS
Optical 300nm – 3000nm
Thermal
>3000nm-
14,000nm
Microwave 1mm-1mCelestial RS
Monday, March 30, 2015Institute of Geology, University of the Punjab
6
HUMAN’s EYE
Rods (to see objects at night) = 7 million
Cones (to see colors) = 100 million
CAT’s EYE
Rods (to see objects at night) =~ 21 million
Cones (to see colors) =~ far less
Monday, March 30, 2015Institute of Geology, University of the Punjab
7
The basic principle of remote sensing is based upon the interaction of
electromagnetic radiation with atmosphere and the earth. Electromagnetic
radiation reflected or emitted from an object is the usual source of remote
sensing data.
Monday, March 30, 2015Institute of Geology, University of the Punjab
8
Remote sensing is
concerned with the
measurement of EMR
returned by the earth’s
natural and cultural
features that first receive
energy from the sun or an
artificial source such as a
radar transmitter.
Visible light contains light
from 0.4 to 0.7 micrometers
Infrared light from 0.1
micrometers to 1 millimeter
Wavelength
Frequency
(how many times peak
passes per second)
Light - can be thought of as a wave in the 'electromagnetic field' of the universe
A wave can be characterized by its wavelength or its frequency
Blue green yellow red
1020 Hz 1018 Hz 1016 Hz 1014 Hz 1012 Hz 1010 Hz
1 pm 10pm 10 nm 1 micron 100 microns 1 mm 100 mm
vi-
si-
ble
Gamma
Rays
X-Rays UV N.
IR
Th.
IR
Microwaves
Radar
TV FM
Radiowaves
0.4 m 0.5 m 0.6 m 0.7 m
Mid
IR
Far IR
Monday, March 30, 2015Institute of Geology, University of the Punjab
9
Types of Remote Sensing
Passive Remote Sensing andActive Remote Sensing
Active Remote SensingPassive Remote Sensing
Remote sensing methods that provide
their own source of electromagnetic
Remote sensing of energy naturally
reflected or radiated from the terrain.
radiation to illuminate the terrain.
Radar is one example.
Own energy source
© 2008 Ko Ko Lwin
Monday, March 30, 2015Institute of Geology, University of the Punjab
10
Monday, March 30, 2015Institute of Geology, University of the Punjab
11
Components in Remote Sensing
Platform
The vehicle which carries a sensor. i.e. satellite, aircraft, balloon, etc...
Sensors
Device that receives electromagnetic radiation and converts it into a signal that can be
recorded and displayed as either numerical data or an image.
One platform can carry more than
one sensor. For example:
Platform
Sensor
Platform Name Sensor Name
Landsat TM Thematic Mapper
(Passive: Optical sensor)
Landsat ETM Enhanced Thematic Mapper
(Passive: Optical sensor)
ALOS PRISM (Passive: Optical sensor)
AVNIR-2 (Passive: Optical sensor)
PALSAR (Active: Microwave sensor)
Monday, March 30, 2015
12
Remote Sensing and GIS Work Flow
Platform (satellite) DATA ACQUISITION
Data transmission
Ground receiving station &
data warehouse
Sun
Solar radiation from
the sun
Earth
1Example in optical Remote Sensing
DATA PROCESSING & ANALYSIS DATA PRE-PROCESSING
Atmospheric correction
Radiometric correction
Geometric correction
etc.Spatial data modeling along
with other GIS dataset
Algorithm development
Multi-spectral classification 23
© 2008 Ko Ko Lwin
Monday, March 30, 2015Institute of Geology, University of the Punjab
13
Examples
Landsat TM/ETM
SPOT
ALOS
IKONOS
QuickBird
Earth rotation
Satellite orbit
Monday, March 30, 2015Institute of Geology, University of the Punjab
14Resolutions
SPATIAL
Smallest identifiable
area as a discrete
object in an image
SPECTRAL
No. of frequencies
recorded = sensors
TEMPORAL
Time interval between
measurements
RADIOMETRIC
Intensities identified
by sensors
Monday, March 30, 2015Institute of Geology, University of the Punjab
15
Serial
No.
Satellites
Altitude
(km)
Bands (µm) Multi-spectral (m)
Panchromati
c (m)
Thermal
(m)
Purpose
Monday, March 30, 2015Institute of Geology, University of the Punjab
16
Monday, March 30, 2015Institute of Geology, University of the Punjab
17
Imagery and their price ranges
Monday, March 30, 2015Institute of Geology, University of the Punjab
18
Imagery free of cost
Monday, March 30, 2015Institute of Geology, University of the Punjab
19

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Lec_13_Introduction to Remote Sensing (RS)

  • 1. Fundamentals of Remote Sensing Prof. Dr. Sajid Rashid Ahmad sajidpu@yahoo.com Atiqa Ijaz Khan _ Demonstrator atiqa_ss09@yahoo.com
  • 2. • What is Remote Sensing? • If you are reading this sentence, now you are doing Remote Sensing. In fact, any information acquired from the object without touching is Remote Sensing. • Remote sensing offers the ability to observe and collect data for large areas relatively quickly, and is an important source of data for GIS. (Source: digimap) Monday, March 30, 2015Institute of Geology, University of the Punjab 2
  • 3. Remote Sensing • “The art and science of obtaining information about an object without being in direct contact with the object” (Jensen 2000). • The science (and art) of acquiring information about an object, without entering in contact with it, by sensing and recording reflected or emitted energy and processing, analyzing, and applying that information. • Information usually gathered from spacecraft or an airplane. • In from of aerial photographs to satellite images. Monday, March 30, 2015Institute of Geology, University of the Punjab 3
  • 4. Monday, March 30, 2015Institute of Geology, University of the Punjab 4 Eyes Binoculars Digital Camera Pigeon Cameras 1903
  • 5. Monday, March 30, 2015Institute of Geology, University of the Punjab 5Types Terrestrial RS Optical 300nm – 3000nm Thermal >3000nm- 14,000nm Microwave 1mm-1mCelestial RS
  • 6. Monday, March 30, 2015Institute of Geology, University of the Punjab 6 HUMAN’s EYE Rods (to see objects at night) = 7 million Cones (to see colors) = 100 million CAT’s EYE Rods (to see objects at night) =~ 21 million Cones (to see colors) =~ far less
  • 7. Monday, March 30, 2015Institute of Geology, University of the Punjab 7 The basic principle of remote sensing is based upon the interaction of electromagnetic radiation with atmosphere and the earth. Electromagnetic radiation reflected or emitted from an object is the usual source of remote sensing data.
  • 8. Monday, March 30, 2015Institute of Geology, University of the Punjab 8 Remote sensing is concerned with the measurement of EMR returned by the earth’s natural and cultural features that first receive energy from the sun or an artificial source such as a radar transmitter. Visible light contains light from 0.4 to 0.7 micrometers Infrared light from 0.1 micrometers to 1 millimeter Wavelength Frequency (how many times peak passes per second) Light - can be thought of as a wave in the 'electromagnetic field' of the universe A wave can be characterized by its wavelength or its frequency Blue green yellow red 1020 Hz 1018 Hz 1016 Hz 1014 Hz 1012 Hz 1010 Hz 1 pm 10pm 10 nm 1 micron 100 microns 1 mm 100 mm vi- si- ble Gamma Rays X-Rays UV N. IR Th. IR Microwaves Radar TV FM Radiowaves 0.4 m 0.5 m 0.6 m 0.7 m Mid IR Far IR
  • 9. Monday, March 30, 2015Institute of Geology, University of the Punjab 9 Types of Remote Sensing Passive Remote Sensing andActive Remote Sensing Active Remote SensingPassive Remote Sensing Remote sensing methods that provide their own source of electromagnetic Remote sensing of energy naturally reflected or radiated from the terrain. radiation to illuminate the terrain. Radar is one example. Own energy source © 2008 Ko Ko Lwin
  • 10. Monday, March 30, 2015Institute of Geology, University of the Punjab 10
  • 11. Monday, March 30, 2015Institute of Geology, University of the Punjab 11 Components in Remote Sensing Platform The vehicle which carries a sensor. i.e. satellite, aircraft, balloon, etc... Sensors Device that receives electromagnetic radiation and converts it into a signal that can be recorded and displayed as either numerical data or an image. One platform can carry more than one sensor. For example: Platform Sensor Platform Name Sensor Name Landsat TM Thematic Mapper (Passive: Optical sensor) Landsat ETM Enhanced Thematic Mapper (Passive: Optical sensor) ALOS PRISM (Passive: Optical sensor) AVNIR-2 (Passive: Optical sensor) PALSAR (Active: Microwave sensor)
  • 12. Monday, March 30, 2015 12 Remote Sensing and GIS Work Flow Platform (satellite) DATA ACQUISITION Data transmission Ground receiving station & data warehouse Sun Solar radiation from the sun Earth 1Example in optical Remote Sensing DATA PROCESSING & ANALYSIS DATA PRE-PROCESSING Atmospheric correction Radiometric correction Geometric correction etc.Spatial data modeling along with other GIS dataset Algorithm development Multi-spectral classification 23 © 2008 Ko Ko Lwin
  • 13. Monday, March 30, 2015Institute of Geology, University of the Punjab 13 Examples Landsat TM/ETM SPOT ALOS IKONOS QuickBird Earth rotation Satellite orbit
  • 14. Monday, March 30, 2015Institute of Geology, University of the Punjab 14Resolutions SPATIAL Smallest identifiable area as a discrete object in an image SPECTRAL No. of frequencies recorded = sensors TEMPORAL Time interval between measurements RADIOMETRIC Intensities identified by sensors
  • 15. Monday, March 30, 2015Institute of Geology, University of the Punjab 15 Serial No. Satellites Altitude (km) Bands (µm) Multi-spectral (m) Panchromati c (m) Thermal (m) Purpose
  • 16. Monday, March 30, 2015Institute of Geology, University of the Punjab 16
  • 17. Monday, March 30, 2015Institute of Geology, University of the Punjab 17 Imagery and their price ranges
  • 18. Monday, March 30, 2015Institute of Geology, University of the Punjab 18 Imagery free of cost
  • 19. Monday, March 30, 2015Institute of Geology, University of the Punjab 19