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Semidiurnal M-2 internal tides in the Indo-Australian Basin

机译:印澳盆地半日M-2内潮

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摘要

Clear signals of internal tide propagation are found at the semidiurnal M-2 frequency in the eastern South Indian Ocean over the abyssal plain of the Indonesian Australian Basin. We find a spatially and temporally coherent internal tide with phase propagation estimated from satellite altimetry suggesting generation along the Indonesian Archipelago and the Australian North West Shelf east of 115 degrees E. A sinusoidal fit is used to estimate internal tide phase and amplitude along vertical cross sections from expendable bathythermograph (XBT) data along volunteer merchant shipping lines. It is likely tidal energy in the middle of the Indonesian Australian Basin is from both northern and southern source regions, and may sustain a second region of enhanced mixing for the Indonesian Throughflow.
机译:在印度洋澳大利亚盆地深渊平原上的南印度洋东部,在半日M-2频率发现了内部潮汐传播的清晰信号。我们发现了一个时空相干的内部潮汐,其相位传播是根据卫星测高仪估算的,这表明沿印度尼西亚群岛和澳大利亚西北大陆架东经115度产生了一个正弦曲线。正弦拟合用于估算垂直剖面上的内部潮汐相位和振幅从自愿性商船运输路线上的消耗性水温仪(XBT)数据中获得。印尼澳大利亚盆地中部的潮汐能可能来自北部和南部源区,并可能为印尼通流维持第二个增强混合的区域。

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