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Monitoring of the Tsushima Warm Current at the Tsushima/Korea Straits

机译:在Tsushima /韩国海峡监测Tsushima热潮

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The research Institute for Applied Mechanics (RIAM), Kyushu University has been conducting long-term acoustic Doppler current profiler (ADCP) observation since February 21, 1997 along the cruise line between Hakata and Pusan to measure the current structure and its time variations at the Tsushima Straits. The Camellia, kitted with a multi-level type ADCP system (VM-BBADCP, 300 kHz, RD Instruments) makes round trips between Hakata and Pusan three times a week at a cruising speed of about 17 kt. The data sampling interval is about 24 seconds and 8 m in depth, from 18 m to 258 m. However the data within the range of 15% of the total depth from the bottom are not of reliable quality (missing data). Since the maximum water depth is about 240 m along the ferry track, the ship velocity relative to the bottom can be measured everywhere through the bottom tracking by the ADCP, implying that the current velocity can be measured relative to the bottom. Constituents of tidal current were decomposed from the observed current data to obtain accurately the mean current without tidal aliasing errors. Using the mean current data, the time variations of the structure and volume transport of the Tsushima current were studied.
机译:九州大学的应用力学研究所(RIAM),自1997年2月21日沿着博多和釜山之间的巡航线进行了长期声学多普勒目前的分析器(ADCP)观察,以衡量当前结构及其时间变化Tsushima海峡。山茶花,带有多级ADCP系统(VM-BBADCP,300 kHz,RD Instruments),在Hakata和Pusan之间的三次以大约17 kt的巡航速度进行三次。数据采样间隔大约24秒,深度为8秒,从18米到258米。然而,来自底部总深度的15%范围内的数据不具有可靠的质量(缺少数据)。由于沿轮渡轨道的最大水深是约240μm,因此可以通过ADCP的底部跟踪到处理地测量相对于底部的船速,这意味着可以相对于底部测量电流速度。潮流的成分从观察到的电流数据分解,以准确地获得平均电流而没有潮汐锯齿误差。使用平均电流数据,研究了Tsushima电流结构和体积传输的时间变化。

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