MODULE :- 1
INTRODUCTION
TO
RS & GIS (BCV515D)
By
1Dr. Tejaswini N. Bhagwat
Associate Professor
Department of Studies in Civil Engineering
BASIC CONCEPT of RS
Humans apply remote sensing in their day-to-day business, through vision, hearing and sense of smell
WHAT IS REMOTE SENSING ?
SCIENCE and ART of obtaining INFORMATION about an OBJECT, AREA or PHENOMENON through the analysis of data acquired by a DEVICE that is not in contact with the object, area or phenomenon under investigation.
OBJECT – Building, Tankers.
AREA - Water bodies, Forest cover, Cultivated land, Rocky area.
PHENOMENON – Forest Fire, Floods, Oil slick, Earthquake, Drought, Erosion, EIA.
DEVICE – Sensors – Active and Passive.
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DATA AND INFORMATION
Type of Remote Sensing
REMOTE SENSING PROCESS
REMOTE SENSING IN INDIA
Applications
Users
Service providers > 200
TELEMEDICINE VIA SATELLITE
Referral �Hospitals
Panel of Doctors
Video Conferencing
Pathology
Cardiology
Video Conferencing
Health Specialist �Centre
Reaching the un-reached
Rural /
Remote/ Inaccessible
Extension education for Doctors in rural/remote areas
IMAGE CORRECTION/
MAP MAKING
NAVIGATION/
LANDING
ROAD NAVIGATION
SHIP ROUTING
POSITIONING AND NAVIGATION
TECHNOLOGY ISSUES
APPLICATIONS
COMMUNICATIONS FOR DEVELOPMENT
MULTI-MEDIA
INFORMATION SERVICES
IRS
INSAT
INTEGRATED SYSTEM
PRIORITY AREAS
TV RECEIVE ONLY TERMINALS
STUDIO/DATA BANK
TALK BACK TERMINAL
SPACE AND AGRICULTURE
DRINKING WATER
FOR NATION
BASE MAP
LITHOLOGICAL MAP
STRUCTURAL MAP
GEOMORPHOLOGICAL MAP
HYDROLOGICAL MAP
HYDRO-GEOMORPHOLOGICAL MAP
Scientific source
finding approach
l
HYDROGEOMORPHOLOGICAL
MAP
SATELLITE IMAGERY
Locating and Recharging Ground Water
Success rate in locating
water up to 95%
OCEAN APPLICATIONS
PFZ Image
PFZ Map
IRS P4 - OCM
Sea Surface Temperature �retrieval from NOAA-AVHRR data
POTENTIAL FISHING ZONE
(IRS P-4 OCM DERIVED)
November 17, 1999
0.1
mg/m3
5.0
Observation No.
Normalized catch �(Kg/operation)
NORMAL CATCH ~ 10 YRS Av.
CATCH AT PFZ
0
100
200
300
400
1
2
3
4
5
6
7
8
9
10
OFF GOA
OFF �GUJARAT
3.0
November 21, 2000
IRS WiFS based NDVI
May-July 2001
Severely drought
affected districts
DROUGHT MONITORING
KARNATAKA PROVINCE
Increasing NDVI
Targeting social safety nets
Relief and Rehabilitation
Subsidy and Entitlements
Developmental focus
NDVI- normalized difference vegetation index
Reporting hierarchy
May-July 2000
SPACE AND URBAN DEVELOPMENT
METEOROLOGICAL APPLICATIONS
DATA COLLECTION SYSTEMS
INSAT-3A
Kalpana-1
1. The interpretation of imagery requires a certain skill level
2. Needs cross verification with ground (field) survey data
3. Data from multiple sources may create confusion
4. Objects can be misclassified or confused
5. Distortions may occur in an image due to the relative motion of sensor and source
6. High cost of satellite systems
7. Takes 10 years + to develop, build, test, and launch
LIMITATIONS
Electromagenetic Energy
ELECTROMAGNETIC SPECTRUM
Fig. : Electromagnetic spectrum
Fig.: Electromagnetic spectrum:COSMOS
Electromagnetic spectrum - wavelength bands
Visible range Blue - 0.4 - 0.5 μm
Green - 0.5 – 0.6 μm
Red - 0.6 – 0.7 μm
Infrared (IR): Near IR - 0.7 – 1.3 μm
Mid IR - 1.3 – 3.0 μm
Thermal IR - beyond 3 μm
Micro wave 1 mm – 1 m
Earth's atmosphere absorbs energy in γ rays, x rays and ultraviolet bands
– not used in Remote Sensing
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ENERGY INTERACTION WITH THE ATMOSPHERE
SCATTERING
Types of scattering
i) Rayleigh scattering.
ii) Mie scattering.
iii) Non selective scattering
ii) Mie scattering occurs when the particles are just about the same size as the wavelength of the radiation.
iii) Non selective scattering the final scattering mechanism of importance is called non selective scattering.
In contrast to the absorption bands, there are areas of the electromagnetic spectrum where the atmosphere is transparent (little or no absorption of radiation) to specific wavelengths. These wavelength bands are known as atmospheric “windows”
Energy interactions with Earth surface features
RESOLUTION
INDIAN IMAGING CAPABILITY
IMAGE REGISTRATION
AIRPORT
IMAGE
IMAGE OF VIDHAN SOUDHA
CHARACTERISTICS OF IMAGES
TECHNIQUES OF INTERPRETATION
Identification of different objects in the scene
(1) Digital interpretation:- Allow for quantitative analysis of all spectral band in imagery simultaneously and is able to detect subtle differences that we cannot.
(2) Visual interpretation: - Does not allow for full exploitation of data provided. A human can only visually interpret three types of remotely sensed information at a time.
ELEMENTS OF VISUAL INTERPRETATION TECHNIQUES
1) Tone refers to the relative brightness or colour of objects in image. Generally, tone is the fundamental element for distinguishing between different targets or features.
2-Shape refers to the general form, structure, or outline of individual objects.
3-Size of objects in an image is a function of scale.
4-Pattern refers to the spatial arrangement of visibly discernible objects.
5-Texture refers to the arrangement and frequency of tonal variation in particular areas of an image.
6-Shadow is also helpful in interpretation as it may provide an idea of the profile and relative height of a target or targets which may make identification easier. However, shadows can also reduce or eliminate interpretation in their area of influence, since targets within shadows are much less (or not at all) discernible from their surroundings. Shadow is also useful for enhancing or identifying topography and landforms, particularly in radar imagery.
7-Association takes into account the relationship between other recognizable objects or features in proximity to the target of interest. The identification of features that one would expect to associate with other features may provide information to facilitate identification. In the example given above, commercial properties may be associated with proximity to major transportation routes, whereas residential areas would be associated with schools, playgrounds, and sports fields. In our example, a lake is associated with boats, a marina, and adjacent recreational land.
Thank You
Fig: Indian Remote Sensing Satellites
Remote Sensing Platform
1.Platform is a stage where sensor or camera is mounted to acquire information about a target under investigation.
2. According to Lillesand and kiefer (2000), a platform is a vehicle, from which a sensor can be operated. For remote sensing applications, sensors should be mounted on suitable stable platforms. These platforms can be ground based, air borne or space borne based.
3. As the platform height increases the observational area increases. Thus, higher the sensor is mounted;large synoptic view is obtained.
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4. The types or characteristics of platform depend on the of sensor to be attached and its application. Depending on task, platform can vary from ladder to satellite.
5. Three types of platforms are used to mount the remote sensors-
Ground Based Platform
1.Sensor installed over ground based platforms records detailed information about the feature or surface area such as a crop field or road intersection of limited extent(i.e 200 to 400 sq. m) which may be compared with information collected from aircraft or satellite sensors as per the required of the researcher.
2. Ground observation platforms include-handheld platform, cherry picker, towers, portable masts and vehicles etc.
3. To study properties of single plant or a small patch of grass, ground based platform is used (hand-held or mounted on a tripod).
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4.For the field investigations, some of the most popular platforms have been used are cherry picker platform, portable masts and towers. The cherry picker platforms can be extended to approximately 15m.
5. They have been used by various laboratories to carry spectral reflectance meters and photographic systems.
6. Portable masts are also available in various forms and can be used to support cameras and sensors for testing.
7. Permanent ground platforms like towers and cranes are used for monitoring atmospheric phenomenon and long-term monitoring of terrestrial features.
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8.Towers can be built on site and can be tall enough to project through a forest canopy so that a range of measurements can be taken from the forest floor, through the canopy and from above the canopy.
2.Air Based Platforms
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4. The speed, altitude as well as orientation of the aircraft must be carefully chosen so as to have minimum influence on the scale, resolution and geometric characteristics of record images.
5. Other airborne observation platforms include ballons, drones (short sky spy) and high altitude sounding rockets. Helicopters are occasionally used.
Balloons
1.Ballons are used for remote sensing observation (aerial photography) and nature conservation studies.Ballon floats at a constant height of about 30km.
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2. It consists of a rigid circular base plate for supporting the entire sensor system which is protected by an insulting and shock proof light casing.
3.The balloon is governed by the wind at the floating altitude. Balloons are rarely used today because they are not very stable and the course of flight is not always predictable, although small balloons carrying expendable probes are still used for some meteorological research.
4.Ballons as platforms are not very expensive like arcrafts. They have a great variety of shapes, sizes and performance capabilities. The balloons have low acceleration, require no power and exhibit low vibrations.
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5.There are three main types of balloon systems, viz.free balloons and powered balloons.
Drones
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4. Drones was developed on britain during world war-II, is the short sky spy which was originally concieved as a military reconnaissance. Now it plays important role in remote sensing.The unique advantage is that could be accurately located above the area for which data was required and capable to provide both night and day data.
3. Aircraft platforms
1. Aerial platforms are primarily stable wing aircraft. Helicopters are also occasionally used for this purpose. Generally, aircraft are used to collect very detailed image.
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2. Special aircraft with cameras and sensors on vibration less platforms are traditionally used to acquire aerial photographs and images of land surface features.
3. While low altitude aerial photography results in large scale images providing detailed information on the terain, the high smaller scale images offer advantage to cover a larger study area with low spatial resolution.
4. Aircraft platforms offer an economical method of remote sensing data collection for small to large study areas with cameras, electronic imagers, across- tack and along-track scanners, and radar and microwave scanners.
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1.Low altitude aircraft: It is most widely used and generally operates below 30000 ft. They have single engine or light twin engine. It is suitable for obtaining image data for small areas having large scale.
2.Hogh altitude aircraft: Includes jet aircraft with good rate of climb, maximum speed, and high operating ceilling.It acquires imagery for large areas(smaller scale).
Rockets as Platforms
1.High altitude sounding rocket platforms are useful in assessing the reliability of the remote sensing techmniques as regards their dependence on the distance from the target is concerned.
2.Ballon have a maximum altitude of approxiamately 37km, while satellites cannot orbit below 120km.High altitude sounding rockets can be used to amoderatebaltitude above terrain. Imageries with moderate synoptic view can be obtained from such rockets for area of some 500000 sq.km perframe.
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3.Prior to use of airplanes, aerial photographs were obtained by rocketing a camera into the sky and then retrieving the camera and film.
4. The high altitude sounding rocket is fired from a mobile launcher. During the flight its scanning work is done from a stable altitude, the payload and the spent motor are returned to the ground gently by parachute enabling the recovery of the data.
5. One most important limitations of this system is to ensure that the descending rocket not going to cause damage.
3. Space Borne Platforms
1. Space borne remote sensing is carried out from the outer space or at an altitude higher than the earth’s atmosphere and utilizes space shuttle or more commonly satellite as platforms.
2. Space borne or satellite platform are onetime cost effected but relatively lower cost per unit area of coverage, can acquire imagery of entire earth without takung permission. Space borne imaging ranges from altitude 250km to 36000km.
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3.Satellites are man made objects that resolve around the earth and sensors installed onboard captures data of earth’s surface covering areas of more than hundreds of sq. km. Because of their orbits, satellites permit repetitive coverage of the earth’s surface on a continuing basis.
4. Ever since the launch of the first earth satellite (i.e Landsat in 1972),satellite based remote sensing has continuously served towards the betterment of science and technology.
There are two types of well recognized satellite platform
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geostationary environmental, communication, televison braodcast, weather and earth observation satellite etc are example of unmanned satellite category.
Space borne remote sensing provides the following advantages:
References
THANK YOU