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Civil - Remote Sensing Techniques and GIS - EMR and Its Interaction With Atmosphere and Earth Material

Wavelength Regions Important To Remote Sensing

   Posted On :  09.08.2016 07:47 pm

1 Ultraviolet or UV 2 Visible Spectrum 3 Infrared (IR)

WAVELENGTH REGIONS IMPORTANT TO REMOTE SENSING:

 

 

1 Ultraviolet or UV

 

For the most purposes ultraviolet or UV of the spectrum shortest wavelengths are practical for remote sensing. This wavelength beyond the violet portion of the visible wavelengths hence it name. Some earth surface materials primarly rocks and materials are emit visible radiation when illuminated by UV radiation.

 

2 Visible Spectrum

The light which our eyes - our "remote sensors" - can detect is part of the visible spectrum. It is important to recognize how small the visible portion is relative to the rest of the spectrum. There is a lot of radiation around us which is"invisible" to our eyes, but can be

 

detected by other remote sensing instruments and used to our advantage. The visible wavelengths cover a range from approximately 0.4 to 0.7 ?m. The longest visible wavelength

 

is red and the shortest is violet. Common wavelengths of what we perceive as particular colours from the visible portion of the spectrum are listed below. It isimportant to note that this is the only portion of the spectrum we can associate with the concept of colours.


Violet: 0.4 -0.446 ?m

 

Blue: 0.446 -0.500 ?m

 

Green: 0.500 -0.578 ?m

 

Yellow: 0.578 -0.592 ?m

Orange: 0.592 -0.620 ?m

 

Red: 0.620 -0.7 ?m

 

Blue, green, and red are the primary colours or wavelengths of the visible spectrum. Theyare defined as such because no single primary colour can be created from the other two, but all other colours can be formed by combining blue, green, and red in various proportions. Although we see sunlight as a uniform or homogeneous colour, it is actually composed of various wavelengths of radiation in primarily the ultraviolet, visible and infrared portions of the spectrum. The visible portion of this radiation can be shown in its component colours when sunlight is passed through a prism, which bends the light in differing amounts according to wavelength.

 

 

3 Infrared (IR)

 

The next portion of the spectrum of interest is the infrared (IR) region which covers the wavelength range from approximately 0.7 ?m to 100 ?m more than 100 times as wide as the

visible  portion.  The  infrared  can  be  divided  into  3  categories  based  on  their  radiation

properties-the reflected near- IR middle IR and  thermal IR.

The reflected near IR covers wavelengths from approximately 0.7 ?m to 1.3 ?m is

commonly used to expose black and white and color-infrared sensitive film.

The middle-infrared region includes energy with a wavelength of 1.3 to 3.0 ?m.

 

The thermal IR region is quite different than the visible and reflected IR portions, as

 

this energy is essentially the radiation that is emitted from the Earth's surface in the form of heat. The thermal IR covers wavelengths from approximately 3.0 ?m to 100 ?m.

 

Microwave

 

This wavelength (or frequency) interval in the electromagnetic spectrum is commonly referred to as a band, channel or region.The major subdivision

 

The portion of the spectrum of more recent interest to remote sensing is the microwave region from about 1 mm to 1 m. This covers the longest wavelengths used for remote sensing. The shorter wavelengths have properties similar to the thermal infrared region while the longer wavelengths approach the wavelengths used for radio broadcasts.

 


Tags : Civil - Remote Sensing Techniques and GIS - EMR and Its Interaction With Atmosphere and Earth Material
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