Datatake ERS-1 July 23, 1994 East China Sea North end of Taiwan island Comment The dark rectangular area (1) marks an upwelling zone. Packets of internal waves (2) within the slick are visible due to clutter and small wavebreaking surmounting the tension of the surface film. Reference Yu. Kravtsov, A.V. Kuz'min, O.Yu. Lavrova, L.M. Mitnik, M.I. Mityagina, K.D. Sabinin, Yu.G. Trokhimovskii, Polarization characteristics of radar images of the traces of internal waves on the sea surface// Earth Observation and Remote Sensing, vol.15, No 6, 2000, pp 909-926. Image |
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