REMOTE SENSING
DEFINITION
The technique of acquiringinformation about an object by recording device(sensor)
i.e. Not in physical contact with theobject by measuring portion of reflected or emittedelectromagnetic radiation from the earth’s surface.
PRINCIPLE OF REMOTE SENSING
PROCESS OF REMOTE SENSING
STAGES IN REMOTE SENSING
1. Energy source
Emission of electromagnetic radiation or EMR (sun/ self emission).
2. Energy Interactions With Atmosphere
Transmission of energy from the source to the surface of the earth as well as ABSORPTION & SCATTERING.
3. Interaction of EMR With the Earth Surface
Reflection & emission transmitted or absorbed by the surface.
4. Recording of Energy by the Remote Sensor
Sensor not in touch with the earth’s surface
5. Sensor Data Output
Data transmission & reception.
6. Data (Image) Processing & Analysis
Extraction of information @ the earth surface features.
7. Application
Extracted information is utilized in decision making for solving problems.
TYPES OF RS
A) Types of RS Based on Source of Energy
1. PASSIVE SENSORS
Remote Sensing systems measuring the naturally available energy ( Solar energy: either reflected or absorbed) are called as Passive Sensors.
2. ACTIVE SENSORS
Remote Sensing systems which provides their own source of energy for illumination are known as ‘Active Sensors’.
e.g.
- SLAR: Side looking airborne radar
- SAR: Synthetic Apareture Radar
B) Based on range of electromagnetic spectrum
1. OPTICAL RS
RS of Visible, NIR,MIR 0.3 um - 3 um.
2. THERMAL RS
RS of emitted radiation 3 um - 5 um. & 8 um - 16 um.
3. MICROWAVE RS
RS in higher wavelength 1mm—1m
ADVANTAGES OF RS
Synoptic View
- Facilitates the study of various earth surface features in their spatial relation to each other.
- Helps to delineate the reqd. features & phenomenon.
Accessibility
Possible to gather information at the area when ground survey is not possible.
e.g. Mountainous areas & foreign areas.
Time conservation
Information at the large area is gathered quickly saving time efforts of human.
Multidisciplinary Applications
Remote Sensing data is processed & used in different disciplines like (Applications og GIS)
- GEOLOGY
- FORESTRY
- LANDUSE
- AGRICULTURE
- DEFENCE
- URBAN PLANNING
- FISHERIES
- CIVIL ENGINEERING
ELECTROMAGNETIC RADIATION
1. WAVE MODEL
2. PARTICLE THEORY
Radiation consists of electrical and magnetic fields perpendicular to each other, moving in wave pattern.
- Wavelength (lambda)
- Frequency (v)
- Amplitude (A)
ELECTROMAGNETIC SPECTRUM
Representing the continuum of EMR arranged on the basis of wavelength and frequency.
Electromagnetic spectrum ranges as…
- Gamma Ray ————— shorter wavelengths
- X-ray
- Ultraviolet
- Visible spectrum ———- 400nm—700nm
- Infrared
- Microwaves
- Radiowaves ————— Longer wavelength
ENERGY INTERACTION WITH THE ATMOSPHERE
Atmosphere affect incoming radiation by
- Scattering:
- Rayleigh scattering
- Mie scattering
- Non selective scattering
- Absorption:
- O3 Ozone
- CO2 Carbon Dioxide
- H2O Water Vapour
- Refraction: Atmospheric layer of varyingclarity, humidity, temperature.
ATMOSPHERIC WINDOWS
- These are the regions in the electromagnetic spectrum for which the atmosphere is transparent.
- These wavelengths are easily transmitted through atmosphere.
- These are useful regions for remote sensing.
REFLECTION CHARACTERISTICS OF EARTH COVER
It may be qualified by measuring the portion of incident energy that is reflected.
Vegetation
- Red & Blue colors are absorbed.
- Green & NIR are reflected.
Water :
- All radiation are absorbed.
- Blue or Blue-Green colors are little reflected.
Soil :
- Depend on Moisture,
- Organic Content,
- Texture,
- Structure,
- Iron Oxide Content etc.
Spectral Reflectance Curves
- Refectance Curves for Fresh Snow
- Refectance Curves for Old Snow and ice
- Refectance Curves for Vegetation
- Refectance Curves for Needleleaf vegetation
- Refectance Curves for Dry Soil
- Refectance Curves for Wet Soil
- Refectance Curves for Turbid Water
- Refectance Curves for Clear Water
SATELLITES & SENSORS
Platform is a stage to mount the camera or sensors to collect informationremotely about an object or surface.
- Ground
- Balloon
- Aircraft
- Space Craft / Satellite
SATELLITE ORBIT
- Path followed by the satellite.
1. GEOSTATIONARY SATELLITE
- Revolve at the speed matching the rotation of the Earth(24 hours).
- Located at very high altitudes about 36000Km
- Are put in the equatorial plane orbiting West to East.
- One satellite can view one-third of the globe.
- Used for weather monitoring & communication (INSAT, V-Sat).
- Geo-Synchronous (Equatorial Orbiting) Satellites : Telecommunications, Weather
2. SUN-SNYCHRONOUS SATELLITE
- Inclined ‘North-South’ orbit.
- Inclination carries the satellite Westward.
- Its track covers each area of the world at a Constant time of the day ( local sun time ).
- Descending pass of sun-synchronous satellites – day
- Ascending pass of sun-synchronous satellites – shadow ( night )
- Payload of passive sensors.
- Active sensors can acquire image in ascending pass also.
Day Pass(Sun-Synchronous) |
Night Pass(Sun-Synchronous) |
|
|
Day Pass : Descending |
Night Pass : Ascending |
SWATH (Two Dimensional Image of Earth Surface For An Area)
Q. What is SWATH?
- As a satellite revolve around the Earth, the sensors see a certain portion of Earth surface known as swath.
- For satellite images it is very wide between 10 -100 Km.
- The apparent Westward shift of satellite ( due to Earth’s rotation ) allows the satellite Swath to cover a new area with each pass.
SWATH STAGES |
SWATH STAGES |
|
|
1. Ground Segment (Recieving Antenna) |
2. Satellite Path (Data Acquisition) |
|
|
3. Successive Paths (Gap between Paths) |
4 Stereoscopic Data Acquisition |
List of Satellites
RESOLUTION
It refers to the system’s ability to Record & Display Fine Details.
In Remote Sensing there are Four Types of Resolution
- Spatial resolution
- Spectral resolution
- Radiometric resolution
- Temporal resolution.
TYPES OF RESOLUTION
Spatial Resolution Diagrams:
DIAGRAM |
SENSOR(Meter) |
|
30m : LS-TM, 80m : LS-MSS |
|
10m : SPOT-PLA, 20m : SPOT-MLA |
MULTISPECTRAL SCANNING
A scanning system that is useful to collect data over a range of wavelengths is called MSS.
Across track scanning |
Along track scanning |
scan lines Perpendicular to motion of system |
scan lines Parallel to motion of system |
SATELLITE IN ORBITS
LANDSAT SATELLITE
NASA (National Aeronautic & Space Administration) launched the LANDSAT series. It is Land Observation Satellite Series.
- RBV :- Return Beam Vidicon.
- MSS :- Multispectral scanner. Across track, 4 spectral band data with 80 meters resolution & 6 bits radiometric resolution.
- TM :- Thematic map per, 7 ban data for 6 bands, spatial resolution of 30 metres & for thermal band, 120 metres,
- ETM :- Enhanced Thematic map per, 8 band data.
- Swath :- 185 Km.
SPOT SATELLITE
- Altitude :- 832 Km.
- Revisit :- 26 days.
Payload
- HRV – High resolution visible sensor.
- PAN mode 10 m
- MSS mode 20 m
- HRVIR – Spot 4 – 10 m resolution
- VEGETATION – Spot 4 – 1.165 Km resolution
INDIAN REMOTE SENSING SATELLITE
OBS. NO. |
MISSIONS |
SENSORS |
ALTITUDE (Km) |
REVISIT (DAYS) |
1. |
IRS-1A |
LISS-I, LISS-II |
904 |
22 |
2. |
IRS-1B |
LISS-I, LISS-II |
904 |
22 |
3. |
IRS-1C |
PAN |
817 |
05 |
|
|
LISS-III |
817 |
24 |
|
|
WIFS |
817 |
05 |
4. |
IRS-1D |
PAN |
817 |
05 |
|
|
LISS-III |
817 |
24 |
|
|
WIFS |
817 |
05 |
5. |
IRS-P2 |
LISS-III |
817 |
24 |
6. |
IRS-P3 |
WIFS |
817 |
05 |
|
|
MOS |
817 |
05 |
|
|
ASTRONOMY |
817 |
05 |
7. |
IRS-P4 |
OCR |
727 |
03 |
|
|
MSMR |
727 |
03 |
INDIAN REMOTE SENSING SATELLITE SENSORS LIST
OBS. NO. |
SENSORS |
SPECTRAL RESOLUTION |
SPATIAL RESOLUTION |
SWATH |
1. |
LISS-I |
4 BANDS |
72.50M |
148 KM |
2. |
LISS-II |
4 BANDS |
36.25M |
074 KM |
3. |
LISS-III |
4 BANDS |
23.50M |
141 KM |
4. |
PAN |
1 BANDS |
05.80M |
070 KM |
5. |
WIFS |
2 BANDS |
188.0M |
810 KM |
REMOTE SENSING SATELLITE AND SENSORS LIST
SATELLITE |
VERSION |
MULTI SPRECTRAL SENSORS |
LANDSAT |
1,2,4,5,7 |
MSS: 2VIS + 2NIR |
LANDSAT |
3 |
MSS: 2VIS + 2NIR + 1 TIR |
LANDSAT |
4,5,7 |
BANDS: 1,2,3,4,5,7 VIS & NIR |
LANDSAT |
4,5,7 |
BANDS: 6 - TIR |
IRS |
1A/1B |
LISS-I/II |
IRS |
1C/1D |
LISS-I/III 4 BANDS: 2VIS+2NIR |
SPOT |
MLA |
3 BANDS |
SPOT |
PLA |
1 BAND (PAN) |
ERS |
|
MICROWAVE SAR |
JERS |
|
MICROWAVE SAR |
SATELLITE DATA RECEPTION,TRANSMISSION & PROCESSING
- There are Three main options for ‘transmitting data acquired by satellite’ to the surface.
- Data can be directly transmitted to the earth if a Ground Receiving Station (GRS) is in the line of sight of the structure.
- Data can be recorded on board the satellite for transmission to a GRS at later time.
- Data can also be relayed to the GRS through the TDRSS( Tracking & Data Relay Satellite System ) which contains series of Geosynchronous, communication satellite.
GRS IN INDIA
GRS is located at Shadnagar. NRSA ( National Remote Sensing Agency ) acquires process, & distribute the satellite data from Indian as well as other satellites.
Data tranmission Stages
Satellite (IRS,LANDSAT, SPOT,NOAA, IKONOS )
to
GRS ( Shadnagar – data in raw digital format )
to
NRSA (processing to correct errors & Convert to standard format )
DIGITAL IMAGE PROCESSING
What is Digital Image Processing
Image Processing is manipulation of the images with the help of a Computer System.
HARDWARE |
SOFTWARE |
MONITOR |
1. Image Processing |
CPU |
2. Image Enhancement |
Secondary Storage Devices |
3. Image Classification |
Floppy Disc, Hard Disc, Scanner etc. |
|
1. IMAGE PROCESSING
Preliminary to the main analysis :-
- Removal of error introduced in the imaging.
- Processes are designed to recognize & compensate for:
Errors,
Noise,
Geometric distortions
which are introduced into the data during the scanning, transmission & recording processes.
PREPROCESSING
- Radiometric corrections
- Atmospheric corrections
- Geometric corrections
Radiometric correction
Radiometric errors are caused by detector imbalance & atmospheric deficiencies.
Radiometric corrections are transmitted on the data in order to remove errors, which are atmospheric correction.
Rediometric corrections are geometrically independent.
Radiometric corrections are also called as Cosmetic corrections
Rediometric corrections are done to improve the appearance of the image.
Examples of Radiometric Correction
- Correction of missing scan line
- Correction for periodic line striping
- Random noise corrections
Atmospheric corrections
True ground-leaving radiance is altered by scattering & hence it needs corrections these corrections are called as Atmospheric corrections.
Geometric corrections
The transformation of remotely sensed images so as it has a scale & projections of a map is called as Geometric correction. Systematic & nonsystematic disorders are corrected in Geometric Correction.
2. IMAGE ENHANCEMENT
Image enhancement technique improves the quality & appearance of an image for human visual analysis & subsequently for machine also.
Common techniques are:
- Contrast stretch
- linear & nonlinear
- Spatial filtering
- Band rationing
- principal component analysis
Photo Interpretation Elements / Image Interpretation Elements
- SIZE
- SHAPE
- SHADOW
- TONE
- COLOR
- TEXTURE
- PATTERN
TONE IMAGE
TEXTURE IMAGE
PATTERN IMAGE
SHADOW IMAGE
3. IMAGE CLASSIFICATION
We normally categorize the objects on the Earth’s surface as forest, agriculture field, river, settlements etc.
Digital Image Classification is the process of assigning pixels to classes. These classes represents regions on the image or map & are identified by the number or symbol.
CLASSIFICATION TYPES
- SUPERVISED
- UN-SUPERVISED
1. SUPERVISED
Supervised Image Classification is the process of known identity (trained pixels ) to classify the pixels, whose identity is not known.
DIFFERENT PHASES IN SUPERVISED CLASSIFICATION
- Appropriate classification scheme for analysis is adopted.
- Selection of representative training site & collection of spectral signatures.
- Evaluation of statistics for the training site spectrum data.
- The statistics are analyzed to select the appropriate features ( bands ) to be used in the classification process.
- Appropriate classification algorithm is selected.
- Classify the image into N classes.
- Statistically analyze & evaluate the classification scheme.
2. UN-SUPERVISED
classifiers do not utilized training data as basis of classification; classes are spectral classes; need of reference data to identify informational value of the spectral class.
Sample area known as training areas. Statistics are calculated for training sites. And every pixels within & outside the training site is assigned to a class or category it most likely resembles.
THERMAL IR SENSING
- Thermal Ranges:3 to 5 and 8 to15 Um.
- Emittance:
- Radiation,
- Day and Night Temperature Changes,
- Emittances of terrain features.
- Radiometers and Scanners (Cooled Detectors):
- Low-Energy,
- Coarse-Resolutions : Spatial and Spectral.
- Day and Night Time Thermal Images:
- Geology,
- Geo-Thermal,
- Volcanic, Fires,
- Thermal pollution, etc.
- Thermal Data:
- Landsat-3 : Band-8,
- Landsat- 4 / 5 : Band 6.
- Day and Night - time.
- Interpretation:
- Cool : Dark (low emittances),
- Hot : Bright (high emittances)
REMOTE SENSING APPLICATIONS
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