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ADCP application for long-term monitoring of coastal water

机译:ADCP在沿海水域长期监测中的应用

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Three kind of application of ADCP is reported for long-term monitoring in coastal sea.(1) The routine monitoring of water qualities. The water quality and ADCP echo data (600 kHz) observed in the long-term are analgzed at MT (Marine Tower) Station of Kansai International Airport in the Osaka Bay, Japan. The correlation between the turbidity and echo intensity in the surface layer is not good because air bubbles generated by breaking wave are not detected by the turbidity meter, but detected well by ADCP. When estimating the turbidity consists of plankton population from echo intensity, the effect of bubbles have to be eliminated. (2) Monitoring stirring up of bottom sediment. The special observation was carried out by using following two ADCP in the Osaka Bay, One ADCP was installed upward on the sea. The other ADCP was hanged downward at the gate type stand about 3 m above from the bottom. At the spring tide, high echo intensities indicating the stirring up of bottom sediment were observed. (3) The monitoring for the boundary condition of water mixing at an estuary. In summer season, the ADCP was set at the mouth of Tanabe Bay in Wakayama Prefecture, Japan. During the observation, water temperature near the bottom showed remarkable falls with interval of about 5~7 d. When the bottom temperature fell, the inflow current with low echo intensity water appears at the bottom layer in the ADCP record. It is concluded that when occasional weak northeast wind makes weak coastal upwelling at the mouth of the bay, the combination of upwelling with internal tidal flow causes remarkable water exchange and dispels the red tide.
机译:据报道ADCP在沿海海域长期监测中的三种应用。(1)常规水质监测。长期观察到的水质和ADCP回波数据(600 kHz)在日本大阪湾关西国际机场的MT(海洋塔)站进行了分析。表层的浊度和回波强度之间的相关性不好,因为由浊波仪检测不到破裂波产生的气泡,而ADCP可以很好地检测到。从回波强度估算浊度由浮游生物组成时,必须消除气泡的影响。 (2)监测底部沉积物的搅拌。通过在大阪湾使用以下两个ADCP进行了特殊观察,其中一个ADCP向上安装在海上。另一个ADCP悬吊在离底部约3 m的门型展台下方。在春季潮汐时,观察到高回波强度,表明底部沉积物被搅动。 (3)监视河口水混合的边界条件。在夏季,ADCP设置在日本和歌山县田边湾口处。在观测过程中,底部附近的水温明显下降,间隔约5〜7 d。当底部温度下降时,具有低回波强度水的流入电流出现在ADCP记录的底部。结论是,当偶尔的东北风弱使海湾口处的海岸上升流减弱时,上升流与内部潮汐流的结合导致显着的水交换并消除了赤潮。

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