VHF帯海洋レーダによる外海性海域における冬季表層流動観測の適用性
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概要
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The fundamental characteristics of the high-resolution ocean radar system with the VHF band under severe winter conditions in the open sea area were evaluated through the field observations in Wakasa Bay. As the results, over 50 percentage of the detection ratio of the horizontal currents by the radar was confirmed in about half of observational domain. The comparison between the current data of the radar and that of the current meter in one-month observation at the close point to Tsuruga Peninsula showed good correlation with a correlation coefficient over 0.7 and the standard error of 5 to 10cm/s. It was also indicated that the currents from surface to 5m below the surface were mainly driven by the wind fluctuation component of the 25.3 hours with the phase of 30 minutes.
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