首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Measurement of tidal and residual currents and volume transport through the Qiongzhou Strait using coastal acoustic tomography
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Measurement of tidal and residual currents and volume transport through the Qiongzhou Strait using coastal acoustic tomography

机译:使用沿海声波层析成像技术测量潮州和剩余潮流以及通过琼州海峡的体积输运

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Quantifying the tidal current and volume transport through the Qiongzhou Strait (QS) is vital to understanding the circulation in the northern South China Sea. To measure the tidal current in the strait, a 15-day coastal acoustic tomography (CAT) experiment was carried out at four acoustic stations in March 2013. The horizontal distributions of the tidal currents were calculated by inverse analysis of CAT data. The diurnal tidal current constituents were found to dominate: the ratio of the amplitudes O-1, K-1, M-2, S-2, and MSF was 1.00:0.60:0.47;0.21:0.11. The residual currents were found to flow westward in the northern QS and turn southward in the southern Q. The residual current velocities were larger in the northern area than in the southern area, with a maximum westward velocity of 12.4 cm s(-1) the northern QS. Volume transport estimated using the CAT data varied between -0.710 Sv and 0.859 Sv, with residual current transport of -0.044 Sv, where negative values indicate westward. We conducted a dynamic analysis of the observations made during the study, which suggested that tidal rectification and sea level difference between the two entrances of the QS are important in maintaining the residual current through the strait. This is the first estimation, from synchronous measurements, of major tidal current constituents, residual currents, and volume transport in this strait. (C) 2015 Elsevier Ltd. All rights reserved.
机译:量化通过琼州海峡(QS)的潮流和流量输送对于了解南海北部的环流至关重要。为了测量海峡的潮流,2013年3月在四个声学站进行了为期15天的沿海声波层析成像(CAT)实验。通过对CAT数据进行反分析,计算了潮流的水平分布。发现昼夜潮流成分占主导地位:振幅O-1,K-1,M-2,S-2和MSF之比为1.00:0.60:0.47; 0.21:0.11。发现残留电流在QS北部向西流动,在QQ南部向南流动。北部的残留电流速度大于南部的速度,最大西向速度为12.4 cm s(-1)。北部QS。使用CAT数据估算的体积输运在-0.710 Sv和0.859 Sv之间变化,剩余电流输运为-0.044 Sv,其中负值表示向西。我们对研究过程中的观测结果进行了动态分析,这表明潮汐整流和QS两个入口之间的海平面差异对于维持通过海峡的剩余水流很重要。这是从同步测量中对该海峡主要潮流成分,剩余电流和体积传输的首次估计。 (C)2015 Elsevier Ltd.保留所有权利。

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