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Remote Sensing. Readings: 27-20 and lecture notes Figures to Examine: 27-20 to 27-23. Examine the Image from IKONOS, 27-23 and compare it with the others. Introduction.
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Readings: 27-20 and lecture notes • Figures to Examine: 27-20 to 27-23. • Examine the Image from IKONOS, 27-23 and compare it with the others.
Introduction • Definition: Remote Sensing is the science of obtaining information about an area, object, or phenomenon through the analysis of data acquired by a device which is not in contact with the object, area, or phenomenon under investigation. • Energy, mainly from the sun, propagates through the atmosphere, reflected or re-emitted from the objects, and recorded by “sensors”.
The Electromagnetic Spectrum • Visible wave lengths are very limited , 0.4 to 0.7 mm, Near IR 0.7 to 1.3 mm, mid IR 1.3 to 3 mm. They both could be recorded on films. • Thermal IR is mainly emitted from an object, needs thermal scanning. • Microwaves are very long waves 1mm to 1m • Most common sensing systems operate in one or several of the visible, IR, or microwave portions of the spectrum. • Energy emitted by the sun is within the visible portion, earth’s emitted energy is within the thermal IR portion.
Spectral Reflectance • The ratio between the reflected energy and the incident energy at a certain wave length. • A certain object will have different spectral reflectance at different wave lengths • Different objects will have different spectral Reflectance at the same wave length • Examples: Deciduous and coniferous trees, vegetation, soil and water. • Why do we see “green”. • What is spectral signature?
Dry soil gray brown Vegetation green Water clear Reflectance % Wavelength µm
Normal Color photo Notice the difference in color between natural vegetation and artificial turf Infrared color photo
Normal B/W photo 0.4 to 0.7 µm Deciduous (needle) and coiffeurs trees (broad leaves) reflect the same Deciduous (needle) trees reflect more, brighter B/W Infrared photo 0.7 to 0.9 µm
Thermal and Multispectral scanners • Thermal scanners will detect the emitted energy in the thermal IR band. • Multispectral scanners will detect the reflected energy in the visible, IR and microwave bands, includes a number of detectors corresponding to the number of bands detected. • Thermal IR multispectral scanners. • Imaging Spectrometry: acquisition in many, very narrow, contiguous spectral bands from visible to mid IR
Earth Resource Satellites • There are several types of satellites above you: communications, remote sensing, GPS, radio and TV, .. • US “LnadSat”: • Ground coverage 185 km x 185 km. Equals to 1600 photos at 1: 20,000 with no overlap. • Sensors: MSS, TM, best resolution: 30 m in black and white, LandSat 7: 15 m • French “Spot”: • Ground coverage is 60 x 60 km • Sensors: High Resolution Visible (HRV). Operates within a limited band width: 0.51 to 0.89. Resolution of 10 m in B/W, spot 5: 2.5m
Spot has a better spatial resolution and less spectral resolution than LandSat • Spot imaging system could be oriented to survey a certain area at a certain time and to produce stereo pairs. • Other available systems, some with higher accuracy Such as IKONOS, figure 27-23, 1 m resolution, and Spin-2 2m resolution. • Quick Bird: Resolution up to 60 cm is commercially available today.
SPOT 10m resolution B/W Image LA, California
2 m resolution satellite image of Giza-Egypt, courtesy of Spin-2
Daytime thermal image Quantico, VA
Nighttime thermal IMAGE HEAT LOSS
Recently plowed fields that reveals the foundation of a 320-m long Roman village in northern France.
Digital Image Processing • What is a digital Image • Basic Operations: • Image rectification and restoration • Image enhancement • Image classification • Data merging