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4 - Central Institute of Brackishwater Aquaculture

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National Workshop-cum-Training on Mdnfonnatio ~d Information Management In Aqu8culture<br />

enough for high geometric resolution measurements. The output <strong>of</strong> a remote<br />

sensing system is usually an image representing the scene being observed. A<br />

further step <strong>of</strong> image analysis and interpretation is required in order to extract<br />

useful information from the image. The human visual system is an example <strong>of</strong> a<br />

remote sensing system in this general sense.<br />

2.1.1 Principles<br />

Remote sensing encompasses the set <strong>of</strong> sensors, platforms, and the data<br />

processing techniques that are used to derive information about the physical,<br />

chemical and biological properties <strong>of</strong> the earth surface features (land and ocean)<br />

and atmosphere using sensor onboard (air craft or balloons) or space borne<br />

(satellite, space shuttles) platforms (Figure 1). The oldest form <strong>of</strong> remote<br />

sensing is aerial photography where the sensor system is the camera and film.<br />

The field <strong>of</strong> remote sensing has grown to include electro-optical sensors in optical<br />

or microwave regions <strong>of</strong> electromagnetic spectrum (Figure 2) bands which<br />

acquire multispectral digital images that can be processed and analyzed by<br />

computers. Many <strong>of</strong> these sensors are on satellites, which regularly orbit the<br />

earth.<br />

In optical Remote Sensing, optical sensors detect solar radiation in the visible<br />

and near infrared wavelength regions (commonly abbreviated as VNIR) reflected<br />

or scattered from the earth, forming images resembling photographs taken by a<br />

camera high up in space. Some remote sensing satellites carry passive or active<br />

microwave sensors. The active sensors emit pulses <strong>of</strong> microwave radiation to<br />

illuminate the areas to be imaged. Images <strong>of</strong> the earth surface are formed by<br />

measuring the microwave energy scattered by the ground or sea back to the<br />

sensors. These satellites carry their own "flashlight" emitting microwaves to<br />

illuminate their targets. The images can thus be acquired day and night.<br />

Microwaves have an additional advantage as they can penetrate clouds. Images<br />

can be acquired even when there are clouds covering the earth surface.<br />

Figure 1. Principle <strong>of</strong> Remote Sensing

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