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Observed Tidal Currents and the Characteristics of Principal Tidal Constituents in the South China Sea Deep Basin in 1997-1999

机译:1997-1999观察了南海深盆地主要潮汐成分的潮流和特点

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Current observations from three moored Autonomous Temperature Line Acquisition System (ATLAS) buoys are analyzed to examine the tidal currents in the upper layer of central deep basin of South China Sea (SCS). Spectrum analysis of current data shows that diurnal and semi-diurnal tidal constituents play an important role in the total current, especially the diurnal tidal constituents. In the northern SCS deep basin, two major diurnal constituents K_1 and O_1 could contribute 33% and 21% to depth averaged current, respectively. From north to south, the magnitude of diurnal tidal constituents to the total current decrease while that of semi-diurnal tidal constituents remain similar. The magnitude, direction and contribution of most tidal currents, except the semi-diurnal tidal current in the northern part, vary significantly with water depth. This indicates that the tidal current is mainly baroclinic in upper layer of SCS deep basin.
机译:分析了三次停泊的自主温度线采集系统(ATLAS)浮标的目前观察,以检查南海中央深盆地上层的潮流(SCS)。目前数据的频谱分析表明,昼夜和半昼夜潮汐成分在总电流,尤其是昼夜潮汐成分中起重要作用。在北部SCS深盆地中​​,两个主要的昼夜成分K_1和O_1可以分别贡献33%和21%至深度平均电流。从北到南,昼夜潮汐成分的大小在半昼夜潮汐成分的总电流下降仍然相似。大多数潮流除了北部半场潮流之外​​,水深除了半场潮流之外​​的大多数潮流。这表明潮流主要是SCS深盆地上层的曲金。

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