1. Surface Remote Sensing Basics
(in context of Electromagnetic Radiation)
Faiza Azam

2. Outline Definition Elements of Remote sensing Sensors and Plaforms
Electromagnetic Radiation Spectrum
Classification of Remote sensing on the basis of Electromagnetic spectrum.
Some talk about Orbits.
Conclusion

3. Definiton:
The techniques for acquisition of information about the features of earth (at different time scales), without any physical contact using devices that use electromagnetic energy, acoustic waves and force fields.
Classified as Active or Passive.
Main Elements of remote sensing
1. A PLATFORM to hold the instrument. 2. A target OBJECT to be observed. 3. An instrument or SENSOR to observe the target .
4. Key element is INFORMATION (Data).

4. REMOTE SENSING ELEMENTS4 1 5 7 2 2 6 3
6 – Interpretation and analysis
5 - Transmission, Reception, and Processing
7 – Application
1 - Energy Source or Illumination
2 - Radiation and the atmosphere
3 - Interaction with the target
4 - Recording of energy by sensor

5. Sensors Active and Passive sensing: Active systems:-
Remote sensing systems that provide their own energy source of illumination.
Measure amplitude as well as the phase of the reflected signal.
Operated any time and cover wavelentghs not provided by sun.

6. Sensors Active and Passive sensing: Passive systems:-
Remote sensing systems that measure naturally available energy
Measure incoherent energy.
For reflective energies, passive sensors can only be used when sun is lluminating earth.

7. Platforms Air borne platforms: Fixed wings aircrafts
Used to collect detailed images (photographic).

8. Satellite Platforms
Remote sensing is conducted from space shuttle or orbiting satellites.
Provide repetitive coverage of earth‘s surface on continuous basis.
Space Shuttle Satellite

9. Energy Spectrum Wavelengths used in Remote Sensing
• Ultraviolet – 0.3 to 0.4 μm
• Visible – 0.4 to 0.7 μm
• Near Infrared – 0.7 to 1.3 μm
• Middle Infrared – 1.3 to 2.8 μm
• Thermal Infrared – 2.4 to14 μm
• Microwave – 1 mm to 1 m

10. Electromagnetic Spectrum
Infomation about
Sun and stars

11. Radio waves Wavelength range: < 1 cm – 10, 100 m.
Transmit radio and t.v. signals.
Radar imaging: Waves are transmitted from a satellite or airplane antenna. The reflected waves (brightness) is used to form an image of the ground in complete darkness or through clouds because as they can pass through clouds and dry desert sand.

12. Microwaves
Wavelengths range: approx. 1 mm (the thickness of a pencil lead) - 30 cm (one foot).
Emitted from the Earth, from objects such as cars and planes, and from the atmosphere.
Two types; Active (scatterometers, alimeters)or Passive(Radiometers)
Can be detected to give information, such as the temperature of the object that emitted the microwaves.

13. Infrared Wavelengths range: approx. 0.7 to 300 µm
NIR ( µm) & SWIR ( µm)  reflected IR, solar rad. refleced from earth‘s surface.
MWIR (3 - 8 µm) & LWIR ( µm)  thermal infrared (heat).
Can be detected to give information, such as reflectance

14. Visible Wavelengths range: 400 - 700 nm
Coincides with the wavelength of greatest intensity of sunlight
great utility for the remote sensing of vegetation and for the identification of different objects by their visible colors.

15. Ultravoilet Wavelengths range: 0.3 µm - 3.0 nm.
Emitted from the sun, most of it is blocked by ozone in the upper atmosphere.
Used extensively in astronomical observatories. Also concerned with the measurement of ozone.

16. Classification of Remote Sensing with respect to Radiation

17. Classification

18. Orbits Geostationary orbits
Satellites (geostationary), at altitudes of approximately 36,000 kilometres, revolve at speeds which match the rotation of the Earth (so seem stationary).
Usage:
Collect information continuously over specific areas. (Weather and communications satellites)
Due to high altitude, some satellites can monitor weather and cloud patterns covering an entire hemisphere of the Earth.

19. Orbits Near Polar Orbits:
Platforms follow an orbit (north-south) which, in conjunction with the Earth's rotation (west-east), Cover most of the Earth's surface. Most such orbits are also sun-synchronous.
Usage:
Being sun synchronous, ensures consistent illumination conditions when acquiring images in a specific season over successive years, or over a particular area over a series of days. So important for monitoring changes

20. Orbits Near Polar Orbits
In near polar orbits, satellite travels northern pole to the southern pole. The paths at poles are called ascending and descending passes, respectively.
For sun-synchronous orbit:
Ascending pass shadowed side of the Earth
Descending pass sunlit side of the Earth

21. Conclusion What is remote sensing in general.
Main elements of remote sensing
Sensors, platforms
Electromanetic spectrum
(used for remote sensing)
Classified remote sensing in terms of wavelengths.
Orbits

22. Future of Remote Sensing