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Indian remote sensing satellite mission
1. A Seminar on
Dated: 24th September 2011
GUIDED BY
MR. B. S. MANJARE
P.G. Department of Geology
Rashtrasant Tukadoji Maharaj Nagpur University, Nagpur
2011 - 2012
2. 1. NARRATIVE
2. SPACE TECHNOLOGIES IN SUPPORT OF NATIONAL POWER
3. TYPES OF SATELLITES & LAUNCH VEHICLES
4. IRS SATELLITE AND ITS CHARACTERISTICS
5. APPLICATIONS IN GEOLOGY
6. SUMMARY
7. REFERENCES
3. NARRATIVE
Period After 1945 Space Research Headed By Dr.
Vikram Sarabhai & Homi Bhabha
In1957, the soviet union successfully launched
first satellite sputnik
In the 1960s, the soviet union enabled ISRO with
close ties.
OBJECTIVE OF ISRO
Design & Development of Satellites
Post launch management of satellite system
Dr. Vikram Sarabhai
4. SPACE TECHNOLOGIES IN SUPPORT OF NATIONAL POWER
prime objective to develop space
technology and application various national
tasks
Support of economy areas like water shade , agriculture, geology, water resource etc.
Establishment of NNRM providing operational remote sensing data services
Indian National Satellites (INSAT) & Indian Remote Sensing (IRS) satellites
6. IRS SATELLITE AND ITS CHARACTERISTICS
Learning phase
Aryabhata (360Kg), Bhaskara-I,II (Remote Sensing)
First indigenous satellite launched July 1980 Rohini1 (40Kg)
with the help of SLV rocket
7. IRS 1A
Launch Date: 17 MARCH 1988
I st in series of Remote Sensing Satellite
Polar sun synchronous orbit from the vostok in
USSR
ORBITAL PARAMETER
Altitude - 904 Km
Inclination - 99 degrees
Local Time - 9:40 A.M
Repetivity - 22 Days
Orbits/day-14
Period -103 minutes
Sensors- LISS-I, LISS-II
Mission completed July 1996
after serving for 8 years
ORBITAL PARAMETERS
IRS-1A
IRS-1B
L. Date 29.08.1991
IRS-P2(L.D:15 OCT.1994)
Resolution: 32.74 meter
Repetivity :24 days
8. LISS - I Sensor
LISS - II Sensor
Linear Imaging Self Scanning Sensors (LISS)
Resolution -72.5 m
Swath -148 km
Repetivity- 22 days
Spectral Bands
0.45 - 0.52 microns (B)
0.52 - 0.59 microns (G)
0.62 - 0.68 microns (R)
Solid state detectors.
Charge Coupled Devices (CCD).
Terrain in the cross track
Detector stored image & form scan lines
Two dimensional picture.
Resolution depends on no. of photo
detector & the swath.
Resolution -36.25 m
Swath -74 x 2 km
Repetivity -22 days
Spectral Bands
0.45 - 0.52 microns (B)
0.52 - 0.59 microns (G)
0.62 - 0.68 microns (R)
0.77 - 0.86 microns
0.77 - 0.86 microns
(NIR)
(NIR)
9. 2nd Generation Satellite
IRS
Large Ground Station Network
1C
1D
On Board Tape Recorder (OBTR) with capacity
Launch Date:19May, 1995
Launch Date:27 Sep, 1997
IRS1C
of 62 Gb, storing data 24 min.
Enhanced Payloads like better Spatial
resolution additional spectral band, improved
repetitively
ORBITAL PARAMETER
Orbit: Polar Sun synchronous
Altitude: 817 Km
Inclination: 98.69 deg
L.Time:10:30 A.M (descending
mode)
Repetivity: 24 Days
Orbits/cycle :341
Period:101.35 min
Sensors: PAN, LISS-III, WiFS
Mission completed
IRS1D
Mission completed
10. IRS1D
IRS1C
Altitude:
817 Km
PANCHROMATIC SENSORS
• 5.8m resolution (Pan
only), 5 day revisit by
tilting the camera
LISS III
• 23.5m and 70m
resolution, 3 spectral
bands V-NIR (23.5m
resolution), 24 day
repeat cycle, swath
141km
WiFS
• 188m resolution,
810km swath, 2
spectral bands, 5 day
revisit
11. Oceansat-1
Launch Date: 26May 1999
first satellite built for Ocean applications
weight 1050 kg orbit by PSLV-C2
Sriharikota.
Two sensor Ocean Colour Monitor (OCM)
Multi - frequency Scanning Microwave
Radiometer (MSMR) for oceanographic
studies.
Extend applications to several newer areas.
Having swath 1420km to 1660km
Mission completed on August 8, 2010
12. 3rd
Generation
Launch Date 17Oct,2003
Launch Date 20 April,2011
Resourcesat-1 & 2
Mission Objectives:
Provide continued remote sensing data for integrated land & water resource
management with enhanced multi-spectral / spatial coverage and stereo imaging.
Further carry out studies improved urban planning, national security, forestry and
disaster management.
13. Resourcesat-1 & 2 Features
ORBITAL PARAMETER
Orbit height : 817 km
Orbit period : 101.35 min
Number of Orbits per day : 14
Local Time Equator crossing : 10.30 a.m.
Payload :
Repetivity (LISS-3) : 24 days (341 orbits)
Revisit (LISS-4) : 5 days
Lift-off Mass : 1,360 kg
Power : Solar Array generating 1250 W
Mission Life : 5 years
14.
15. CARTOSAT-1 (IRS P5)
Mission Objectives:
design & develop stereo
imaging & cartographic
applications.
stimulate areas of user
applications in urban
management, mineral
exploration, & disaster
management
Launch date 5 May,2005
ORBITAL PARAMETER
Orbital Altitude :
618 km
Inclination :
97.87 degree
Local time:
10:30 AM
Revisit
: 5 days
Repetition:
126 days
Orbits/day:
14
Period
: 97minutes
Payload: two PAN sensors
16. PAN SENSOR
Stereo viewing
2.5 m resolution
50
Fore look
260
Facility for across track tilt to
give better revisit
Aft look
17. 4th Generation
Cartosat-2
ORBITAL PARAMETER
Altitude: 630 km
Period: 97.4 min.
Time descend : 9.30 am
Orbits/day: 14
Revisit: 4 days
Repitivity: 310 day
Power: solar array
Pay load: PAN
Launched 1/10/07
Operational life: 5 years
PAN specification
Resolution : better than 1mt
Swath: 9.6 km
Spectral band: 0.5-0.85 mm
Solid state recorder: 64 GB capacity for image storage
An advance sensor to give specific spot imagery.
Images use- detailed mapping, infrastructure development & management
Land Information System (LIS) & Geographical Information System (GIS).
18. APPLICATION IN GEOLOGY
Used for resources survey and management under National Natural
Resources Management System (NNRMS) various application are:
Drought monitoring based on vegetation condition.
Flood risk zone mapping
Hydro-geomorphologic maps
Irrigationarea status monitoring
Land use and land cover mapping
Mineral Prospecting
Coastal studies
Forest survey
19. SUMMARY
Synoptic View: high altitude very large area from a narrow
look angle to recognize large structural pattern.
Repetitive coverage: routinely monitoring of changes and
seasonal effect studies.
Uniformity
over time: passes over the given area at
approximately same time of the day and hence repetitive
coverage is obtained. It gives valuable uniformity
Uniformity
over vast area: coverage in every direction
possible to compile mosaic images of good consistency and
accuracy for vast areas
20. REFERENCES
Assefa M. Melesse et.al. (2007), Remote Sensing Sensors and Applications in Environmental
Resources Mapping and Modeling, Sensors, 7, 3209-3241
Dr. Ravi Prakash Gupta(2008), Remote Sensing Geology- 2--th Edition, Germany:
Springer-Verlag Heidelberg, 53-121
Joseph. G. (1996), Imaging sensors for remote sensing, Remote Sensing Rev.13, 257–342.
Josea Sobrino et.al. (2004), Land surface temperature retrieval from LANDSAT TM 5,
Journal of Remote Sensing of Environment, 90, 434-440
K kasturirangan (1995), “present scenario and future thrusts”, Journal of the Indian Society
of Remote Sensing, 23(1), 1-6
Saumitra Mukherjee (2008), Role of Satellite Sensors in Groundwater Exploration, School
of Environmental Sciences, New Delhi. Sensors, 8, 2006-2016
Paul J Curran (1985), Principles of Remote Sensing, London & New York: library of
congress catalog Longman group Ltd., 130-226
Ranganath R. Navalgund, V. Jayaraman, P. S. Roy (2007), Remote sensing applications:
An overview, CURRENT SCIENCE, 93(12)25, 1747-1766
Sylvie Soudarissanane etc. (2011), Scanning geometry: Influencing factor on the quality of
terrestrial laser scanning points, ISPRS Journal of Photogrammetry and Remote Sensing, 66,
389–399
21. SSTO
INDAIN SPACE MISSION : ROAD MAP
System
2025
2015
Thermal
Protection
Systems
Satellite with
replaceable
Power
& Propulsion
2010
Inflatable Antenna
GSLV- MkII
2005
Newer
Bands
SRE
2001 ..
GSLV
PSLV
93 ..
INSAT Series
IRS Series
Multi platform
Multi parameter
Multi resolution
Astrosat
Thank you……
Notas del editor
Aerial photography can be defined as the science of taking a photo from a point in the air, for the purpose of making some type of study of earth. Terrestrial photo – Camera axis is horizontal or near horizontal Aerial photo – Camera axis is vertical or near vertical.Aerial photographs were the first form of Remote Sensing and they still remain most widely used images on even today also.Limitations / Drawbacks of aerial photographs:1. Scale is not uniform. It varies from strip to strip, photograph to photograph and also in same photo at different points.2. Minor structural features such as folds, small scale joints, fractures, lineation, foliation, crossbedding, ripple marks, etc. can not be interpreted unless the scale of photographs is sufficiently large to represent them photographically.3. In some cases exact rock identification may become difficult as rock exposures may be covered by surficial cover, soil, vegetation etc.4. Photo interpretation tells only about those features which are on the surface of Earth.5. Photographic remote sensing is restricted to 0.3 to 0.9 μm region of electromagnetic spectrum and longer wavelength’s valuable information is omitted.6. Photography is restricted by weather, lighting conditions and atmospheric effects.7. Information is recorded in the analog mode / non-digital format. In order to be computer processed, photos must be converted in to digital format although digital cameras are developed and are now used to acquire aerial photographs.
Aerial photography can be defined as the science of taking a photo from a point in the air, for the purpose of making some type of study of earth. Terrestrial photo – Camera axis is horizontal or near horizontal Aerial photo – Camera axis is vertical or near vertical.Aerial photographs were the first form of Remote Sensing and they still remain most widely used images on even today also.Limitations / Drawbacks of aerial photographs:1. Scale is not uniform. It varies from strip to strip, photograph to photograph and also in same photo at different points.2. Minor structural features such as folds, small scale joints, fractures, lineation, foliation, crossbedding, ripple marks, etc. can not be interpreted unless the scale of photographs is sufficiently large to represent them photographically.3. In some cases exact rock identification may become difficult as rock exposures may be covered by surficial cover, soil, vegetation etc.4. Photo interpretation tells only about those features which are on the surface of Earth.5. Photographic remote sensing is restricted to 0.3 to 0.9 μm region of electromagnetic spectrum and longer wavelength’s valuable information is omitted.6. Photography is restricted by weather, lighting conditions and atmospheric effects.7. Information is recorded in the analog mode / non-digital format. In order to be computer processed, photos must be converted in to digital format although digital cameras are developed and are now used to acquire aerial photographs.
Aerial photography can be defined as the science of taking a photo from a point in the air, for the purpose of making some type of study of earth. Terrestrial photo – Camera axis is horizontal or near horizontal Aerial photo – Camera axis is vertical or near vertical.Aerial photographs were the first form of Remote Sensing and they still remain most widely used images on even today also.Limitations / Drawbacks of aerial photographs:1. Scale is not uniform. It varies from strip to strip, photograph to photograph and also in same photo at different points.2. Minor structural features such as folds, small scale joints, fractures, lineation, foliation, crossbedding, ripple marks, etc. can not be interpreted unless the scale of photographs is sufficiently large to represent them photographically.3. In some cases exact rock identification may become difficult as rock exposures may be covered by surficial cover, soil, vegetation etc.4. Photo interpretation tells only about those features which are on the surface of Earth.5. Photographic remote sensing is restricted to 0.3 to 0.9 μm region of electromagnetic spectrum and longer wavelength’s valuable information is omitted.6. Photography is restricted by weather, lighting conditions and atmospheric effects.7. Information is recorded in the analog mode / non-digital format. In order to be computer processed, photos must be converted in to digital format although digital cameras are developed and are now used to acquire aerial photographs.
Aerial photography can be defined as the science of taking a photo from a point in the air, for the purpose of making some type of study of earth. Terrestrial photo – Camera axis is horizontal or near horizontal Aerial photo – Camera axis is vertical or near vertical.Aerial photographs were the first form of Remote Sensing and they still remain most widely used images on even today also.Limitations / Drawbacks of aerial photographs:1. Scale is not uniform. It varies from strip to strip, photograph to photograph and also in same photo at different points.2. Minor structural features such as folds, small scale joints, fractures, lineation, foliation, crossbedding, ripple marks, etc. can not be interpreted unless the scale of photographs is sufficiently large to represent them photographically.3. In some cases exact rock identification may become difficult as rock exposures may be covered by surficial cover, soil, vegetation etc.4. Photo interpretation tells only about those features which are on the surface of Earth.5. Photographic remote sensing is restricted to 0.3 to 0.9 μm region of electromagnetic spectrum and longer wavelength’s valuable information is omitted.6. Photography is restricted by weather, lighting conditions and atmospheric effects.7. Information is recorded in the analog mode / non-digital format. In order to be computer processed, photos must be converted in to digital format although digital cameras are developed and are now used to acquire aerial photographs.
Aerial photography can be defined as the science of taking a photo from a point in the air, for the purpose of making some type of study of earth. Terrestrial photo – Camera axis is horizontal or near horizontal Aerial photo – Camera axis is vertical or near vertical.Aerial photographs were the first form of Remote Sensing and they still remain most widely used images on even today also.Limitations / Drawbacks of aerial photographs:1. Scale is not uniform. It varies from strip to strip, photograph to photograph and also in same photo at different points.2. Minor structural features such as folds, small scale joints, fractures, lineation, foliation, crossbedding, ripple marks, etc. can not be interpreted unless the scale of photographs is sufficiently large to represent them photographically.3. In some cases exact rock identification may become difficult as rock exposures may be covered by surficial cover, soil, vegetation etc.4. Photo interpretation tells only about those features which are on the surface of Earth.5. Photographic remote sensing is restricted to 0.3 to 0.9 μm region of electromagnetic spectrum and longer wavelength’s valuable information is omitted.6. Photography is restricted by weather, lighting conditions and atmospheric effects.7. Information is recorded in the analog mode / non-digital format. In order to be computer processed, photos must be converted in to digital format although digital cameras are developed and are now used to acquire aerial photographs.