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                                                                   Remote Sensing
                     mental  monitoring satellites, there  are  a host  of  fine  spatial  resolution
                     satellites that owe their heritage to the pioneering work done by NASA’s
                     Landsat and Seasat satellites. These satellites employ electronic cameras
                     and special radars to observe the earth and its oceans in great detail for
                     military, scientific, and commercial purposes.
                       Remote sensing from space can be categorized in a variety of different
                     ways,  such  as  the  type  of  sensor  employed,  the  application purpose,
                     and/or the sponsorship of the mission. These themes will be expanded in
                     the sections that follow but are first outlined in this introduction.


                     Sensors


                       Sensors can first be categorized as being passive or active. A passive
                     sensor receives information from the earth and the atmosphere. A camera
                     is a good example of a passive sensor relying on solar illumination of the
                     object(s) in view to provide input to the camera. By contrast, an  active
                     sensor provides the source of  energy used to view  the area of  interest.
                     Radars and lasers are examples of active sensors.

                       Both passive and active sensors operate over a wide portion of the elec-
                     tromagnetic spectrum, The precise frequencies or wavelengths chosen are a
                     function of  first, the application, and second, the influence of the propaga-
                     tion path between the satellite and the earth. The signatures provided by the
                     earth and its atmosphere result from highly complex interactions of induced,
                     in the case of an active sensor, or natural, in the case of  a passive sensor,
                     electromagnetic  radiation.  These  interaction  mechanisms  include
                     reflectance, emission, absorption, and scattering, and the proper blend of
                     sensor wavelengths can reveal information about the types and condition of
                     soil, vegetation, water, ice, and the atmosphere. One of the most popular
                     regions of  the electromagnetic spectrum employed by  remote sensors are
                     the visible bands that provide picture-like observations of the earth’s surface
                     and the clouds that envelope the earth. However, many other portions of the
                     electromagnetic spectrum are used to provide additional information about
                     the earth and its resources. Infrared and microwave sensors provide infor-
                     mation  on  atmospheric,  surface,  and  even  subsurface  conditions.
                     Microwave sensors have the  added benefit of  being  able to  observe the
                     earth’s surface through clouds and the capability of operating day or night.
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