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Mapping tidal current structures in Dalian Bay, China, using coastal acoustic tomography

机译:映射潮流结构,在中国大连湾,使用沿海声学断层扫描

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Eleven sets of coastal acoustic tomography (CAT) systems were successfully deployed in Dalian Bay (DLB) during March 7-8, 2015, aiming to reconstruct the tidal current fields. The number of successful reciprocal transmission lines was 51, which may be the maximum number in ocean acoustic tomography history. The inverse method results showed that the velocity amplitudes in DLB were 0.75 ms-1 near the bay mouth and 0.30 ms-1in the inner bay. Furthermore, the travel time difference data were also assimilated into the Finite-Volume Community Ocean Model based on the ensemble Kalman Filter method. The assimilation showed similar results to those of the inverse method. Both the inverse method and data assimilation effectively reconstructed the tidal current, with a mean root mean square difference of 0.05 ms-1when compared to the Acoustic Doppler Current Profile data. Meanwhile, a tidal vortex west of Dasanshan Island was more effectively shown by assimilation rather than inversion.
机译:2015年3月7日至8日在大连湾(DLB)成功部署了11套沿海声学断层扫描(CAT)系统,旨在重建潮流现场。成功互惠传输线的数量为51,这可能是海洋声学层析造影历史中的最大数量。逆方法结果表明,DLB中的速度幅度为0.75毫秒 -1 靠近海湾嘴和0.30毫秒 -1 在内海湾。此外,旅行时间差数据也基于集合卡尔曼滤波方法同化到有限卷社区海洋模型中。同化显示与逆方法的结果相似。逆方法和数据同化都有效地重建了潮流,平均均方均为0.05毫秒 -1 与声学多普勒电流分布数据相比。与此同时,通过同化而不是反转,更有效地表现出Dasanshan岛以西的潮汐涡流。

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