作者: Gao Shu , A. F. Velegrakis , M. B. Collins
DOI: 10.1007/BF02846616
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摘要: At a shallow water station (6 m in depth), an internal oscillation event which consisted of one or two wave-like features, with period 3 h and height 1.5 m, was observed. The velocities within the column were modified by during flood phase tide; multilayered velocity structure intense shear generated. Further investigations are required to understand fully mechanism for formation such event.