Water is good radar reflector. It reflects radar better than rock (Svitil 1997). Romeiser (2004) states that microwave (radar wavelength) has penetration in sea water only in the order of millimeter only. Hence, water doesn’t pretty much absorb radar energy. That is quite strange as we know that Infrared wavelength will almost 100% be absorbed by water. How much percentage water reflects radar wave is not clearly defined however.
Cambpell (1996) mentions that smooth ocean surface, which has smaller waves rather than radar wavelength, appears dark regions on the image. Radar energy is reflected away from the sensor. Lillesand & Kiefer (1994) also have the same finding that smooth water surface makes no reflectance returns to the sensor. However, coarse water surface may returns radar wave. Furthermore they mention if water surface is roughened by the wind, it will appear lighter tone on radar image. On the other hand, oil spill on the ocean’s surface have a dampening effect on water’s wave, thus appearing darker on radar image because calm water surface has a greater specular reflection than surrounding water.
Therefore, the response of the ocean to radar energy depends on its surface. Figure 1 above shows simplification of radar reflectance on seawater. Figure (1.a) will produce bright radar image because it gives some reflectance back to the sensor. Figure (1.b) will produce dark radar image because it reflects radar signal away from the sensor.
Fortunately – even we can’t use radar to penetrate sea water – there is correlation between radar image appearance and seafloor depth. Lillesand & Kiefe (1994) mention that by observing refraction of waves in shallow water, water depth can be predicted. Another study by Romeiser (2004) reveals an algorithm between radar (InSAR-derived) currents and known water depth from echosoundings. Resulted regression function is used to predict water depth from the currents at other points. Though, that regression should be considered only works locally.
In summary, most radar energy will be reflected by water. Ocean surface response to radar depends on its roughness. Calm seawater will reflect radar away from satellite and rough seawater will reflect some radar energy back to satellite (sensor). Since there is strong relationship between wave refraction and water depth, we can regress the seawater’s roughness (observed by radar) and reference points depth (which its depth is known by sounding). Finally, the observer can predict the depth of certain area, and therefore seafloor terrain using that regression.
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