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TheImprovement ofTropical and Subtropical Rangelands

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84 IMPROVEMENT OF TROPIOAL AND SUBTROPIOAL RANGELANDS<br />

Remote Sensing<br />

Although maps <strong>and</strong> estimates of l<strong>and</strong> characteristics can be produced<br />

by ground sampling alone, it is seldom done for a resource<br />

assessment because of the expense <strong>and</strong> the likelihood of missing important<br />

features.<br />

Remote sensing is the most commonly used tool for gathering<br />

information for large areas. .AIJ defined here, remote sensing includes<br />

the uses of aerial photography <strong>and</strong> satellite imagery to study the<br />

earth's surface. Remote sensing data are unique because they (1)<br />

provide a comprehensive picture <strong>and</strong> permanent record of surface<br />

conditions at one point in time <strong>and</strong> (2) present a vertical perspective<br />

in which all features are represented, essentially in their true geometric<br />

relationship with all other features. There is no ideal remote<br />

sensing system. Thus, a primary task in remote sensing is to select a<br />

system that best meets the needs of the project.<br />

Principlea of Remote Senftn, Remote sensing exploits the difFerences<br />

that can be detected among surface features on an image of the<br />

earth. The ability to distinguish among features is conditioned by<br />

several factors. Foremos~ in many applications is the feature's tone<br />

or color. Earth materials reflec~ or emit electromagnetic radiation,<br />

including light, in different ways (figure 4(2). For example, vegetation<br />

has a unique pattern of reflectance, with moderate reflectance<br />

in the green part of the spectrum, low reflectance in the red part<br />

of the spectrum, <strong>and</strong> very high reflectance in the infrared part of<br />

the spectrum that is just beyond what is visible to the human eye.<br />

Second are ~hose inherent properties of a feature that determine how<br />

it appears, or what is sometimes called a feature's "signature" or "response."<br />

The characteristic shape of a surface feature when viewed<br />

from above (for example, a folded geologic structure) or its relative<br />

size (such as tree versus shrub) are two such properties. Other important<br />

characteristics are less obvious, such as a feature's "texture"<br />

on an image (say the difference between the smooth texture of a<br />

meadow <strong>and</strong> the rough texture of a forest canopy), or the association<br />

of one feature with others (such as pine forests on steep north-facing<br />

mountain slopes).<br />

The type ofremote sensing system used also affects the ability to<br />

distinguish among earth features. Scale-the relationship between<br />

the size of the image <strong>and</strong> the area on the ground it portrays-largely<br />

determines w~at can be seen, especially if geometric properties such

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