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TheImprovement ofTropical and Subtropical Rangelands

TheImprovement ofTropical and Subtropical Rangelands

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86 IMPROVEMENT OF TROPICAL AND SUBTROPICAL RANGELANDS<br />

a "multispectral" approach by examining several different parts of<br />

the spectrum. The value of this approach is easily appreciated when<br />

comparing a black-<strong>and</strong>-white panchromatic photograph with a color<br />

photograph. Color photography provides much more information<br />

than black-<strong>and</strong>-white, but it tends to have poorer spatial resolution,<br />

is more expensive, <strong>and</strong> is difficult to process in some parts of the<br />

world because of the lack of proper equipment.<br />

There is much information outside the visible spectrum that<br />

would be useful for studying vegetation (table 4(1). Photographic<br />

films have been developed that are sensitive to infrared radiation<br />

that is just beyond the visible part of the spectrum. Color infrared<br />

(Cm) film is the most common type. To record infrared energy<br />

using conventional photographic technology, colors from the natural<br />

environment are assigned to other colors on the cm film. Thus, the<br />

final product is sometimes called a false color image: blue is filtered<br />

out, green is recorded as blue, red is recorded as green, <strong>and</strong> infrared<br />

is recorded as red. Because plants reflect more infrared light than<br />

green light, green vegetation appears as various shades of red or<br />

pink. Red soils are yellowish-green, <strong>and</strong> urban areas are bluish-gray.<br />

cm photography is especially effective for mapping vegetation, but<br />

is expensive <strong>and</strong> sometimes difficult to expose <strong>and</strong> process.<br />

Nonphotographic sensing systems can be carried by aircraft <strong>and</strong><br />

spacecraft <strong>and</strong> provide similar kinds of spectral information. Nonphotographic<br />

systems have a number of advantages. For example,<br />

parts of the spectrum that are critical in some applications <strong>and</strong><br />

that are beyond the capability of photographic systems, such as the<br />

thermal <strong>and</strong> microwave (radar), can be sampled. Also, many nonphotographic<br />

systems record images digitally, which allows several<br />

processing options (see below). With the exception of L<strong>and</strong>sat satellite<br />

data, however, nonphotographic imaging systems will be used in<br />

few resource assessments because of the expense of processing <strong>and</strong><br />

the need for special computer facilities.<br />

Satellite Systems Since 1972, satellite imagery suitable for l<strong>and</strong> resource<br />

assessments has been produced continuously for most parts of<br />

the world. L<strong>and</strong>sat was the first satellite to provide regular <strong>and</strong> universal<br />

image data <strong>and</strong> continues to be the most widely used system.<br />

The primary instrument on L<strong>and</strong>sat is the Multispectral Scanner<br />

(MSS), which records images of the earth in four spectral b<strong>and</strong>s (see<br />

table 4(1). Images are recorded digitally but are produced in both<br />

digital <strong>and</strong> photographic formats. The MSS creates an image by<br />

recording the relative brightness of each element or cell of a large

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