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Fundamentals of Remote Sensing |
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5.6.1 Did You Know?"...I like my eggs on ice..." Creating an Ice Chart Once you understand the meaning of the various codes, the interpretation of the ice charts is relatively easy. For more detailed information about the coding procedure and terminology, go to the Canadian Ice Service homepage. Case study (example) The ScanSAR image covered the entire extent of the route, from Resolute Bay on Cornwallis Island to the pole (78°6'N, 104°3'W). The resolution of 100m provided information about the ice cover and type, and mapped coastlines were added following geometric processing, to provide a geographic reference. The team was also equipped with GPS and communication technologies. On the image map, passable ice appears uniformly dark, due to the specular reflection of incident radiation from the radar on the smooth surface. Rubbly, rough ice that often contained enough relief to make skiing impossible appears bright, due to the reflection of the radar energy back to the sensor. The team using RADARSAT image maps was the only one to complete their journey to the magnetic North Pole. The other teams were hindered by rough ice and could not efficiently plan their route without the synoptic view provided by remote sensing. RADARSAT, with its sensitivity to ice type, far northern coverage, and reliable imaging was the most suitable sensor for this type of application. Its success bodes well for future exploration endeavors! Reference: Lasserre, M., 1996. RADARSAT Image Maps Make Arctic Expedition a Success, Remote Sensing in Canada, Vol. 24, No. 1, June, 1996. Natural Resources Canada. Expedition Web Site: http://www.jeaneudes.qc.ca/ |
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