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首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >Variability of nonlinear internal waves in the South China Sea affected by the Kuroshio and mesoscale eddies
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Variability of nonlinear internal waves in the South China Sea affected by the Kuroshio and mesoscale eddies

机译:黑潮和中尺度涡对南海非线性内波的变化性

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Long-term observations of nonlinear internal waves in the South China Sea reveal seasonal to interannual variability. During two selected segments of inverted echo sounder observations, tidal forcing in Luzon Strait is almost identical, but the observed amplitudes of nonlinear internal waves in the South China Sea are very different. The effects of the Kuroshio and mesoscale eddies, reproduced by HYbrid Cooridnate Ocean Model (HYCOM) reanalysis simulation, are then investigated. The Kuroshio can enhance the zonal tilt of the thermocline and induce intruding flow in Luzon Strait. During the two selected segments, different thermocline slopes did not significantly change the internal tide generation, but the intruding flow may result in a 11% difference in the amplitude of generated M_2 internal tides. During the two selected segments, mesoscale eddies appeared on the path of internal wave propagation, a cold eddy in one case and a warm one in the other. The eddies changed local stratification and induced additional background currents, thus affecting the nonlinear evolution of internal tides. In addition, wave front steering due to the mesoscale eddies dramatically affected the observed amplitude changes of the nonlinear internal waves: the edge, rather than the center, of the nonlinear internal wave front passed through the observational stations, resulting in reduced amplitude in the observations.
机译:对南中国海非线性内波的长期观测揭示了季节到年际的变化。在反向超声测深仪观测的两个选定部分中,吕宋海峡的潮汐强迫几乎相同,但在南中国海观测到的非线性内波振幅却大不相同。然后研究了混合坐标系海洋模型(HYCOM)再分析模拟所复制的黑潮涡旋和中尺度涡旋的影响。黑潮能增强温跃层的带状倾斜并诱发吕宋海峡的侵入流。在两个选定的段中,不同的温跃层斜率不会显着改变内部潮汐的产生,但是侵入流可能导致所产生的M_2内部潮汐的振幅相差11%。在这两个选定的部分中,中尺度涡旋出现在内波传播的路径上,一种情况是冷涡流,另一种情况是热涡流。涡流改变了局部分层并引起了额外的背景电流,从而影响了内部潮汐的非线性演化。此外,由于中尺度涡旋引起的波前转向极大地影响了所观测到的非线性内波振幅变化:通过观测台站的非线性内波前的边缘而不是中心,从而导致观测振幅减小。

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