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Comparisons between measured and theoretical results for C- and Ku-bands backscatter from naturally occurring internal wave current patterns

机译:自然发生的内部波电流模式对C和Ku波段反向散射的测量结果与理论结果之间的比较

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摘要

Predicted and measured values of radar backscatter and of internal wave surface currents are compared using data obtained during the SCATTMOD internal wave experiment. Radar backscatter and surface truth measurements were obtained during six days in August 1985 and cover nine sets of tide-generated internal waves in the Georgia Strait, Canada. The radar portion of this data consists of approximately 75 sets each of C- and Ku-band fanbeam airborne scatterometer signals, each processed to 25 incidence angles and an along-track resolution of either 12.5 or 6.25 m. Aircraft navigation data were also recorded, simultaneous surface measurements, including wave slope, wave height, current, wind, and ship position, were obtained from the CFAV Endeavour. Current meter were located both fore and aft to allow internal wave-phase velocity estimates to be computed.
机译:使用在SCATTMOD内部波实验期间获得的数据,比较了雷达反向散射和内部波表面电流的预测值和测量值。 1985年8月的6天中,获得了雷达的反向散射和地表真值测量结果,覆盖了加拿大乔治亚海峡的9组潮汐产生的内波。该数据的雷达部分包括大约75组C波段和Ku波段扇形光束机载散射仪信号,每个信号处理为25个入射角,并且沿航迹的分辨率为12.5或6.25 m。还记录了飞机导航数据,同时从CFAV奋进号获得了同时的水面测量结果,包括波浪坡度,波浪高度,水流,风向和船舶位置。电流表位于前后,可以计算内部波速。

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