Observation of a shallow water internal oscillation event

Gao Shu; A. F. Velegrakis; M. B. Collins

doi:10.1007/BF02846616

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Observation of a shallow water internal oscillation event

Updated：2023-05-16

- Observation of a shallow water internal oscillation event
- Journal of Oceanology and Limnology Vol. 20, Issue 1, Pages: 86-90(2002)
- Affiliations：
  
  1. Institute of Oceanology Chinese Academy of Sciences
  2. School of Ocean and Earth Sciences The University
- Author bio：
- Funds：
- DOI：10.1007/BF02846616
  CLC：
- Published：2002
- Accepted：
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Shu, G., Velegrakis, A.F. & Collins, M.B. Observation of a shallow water internal oscillation event., Chin. J. Ocean. Limnol. 20, 86–90 (2002). https://doi.org/10.1007/BF02846616
DOI：

Shu, G., Velegrakis, A.F. & Collins, M.B. Observation of a shallow water internal oscillation event., Chin. J. Ocean. Limnol. 20, 86–90 (2002). https://doi.org/10.1007/BF02846616 DOI：

摘要

Abstract

At a shallow water station (6 m in depth)

an internal oscillation event which consisted of one or two wave-like features

with a period of 3 h and a height of 1.5 m

was observed. The velocities within the water column were modified by the event during the flood phase of the tide; a multilayered velocity structure and intense shear were generated. Further investigations are required to understand fully the mechanism for the formation of such an event.

关键词

Keywords

references

Huthnance, J. M., 1989. Internal tides and waves near the continental shelf edge.Geophysical and Astrophysical Fluid Dynamics 48: 81–106.

Lighthill, J., 1978. Waves in Fluids. Cambridge University Press, Cambridge, 504p.

Roberts, J., 1975. Internal Gravity Waves. Marcel Dekker, New York, 274p.

Thorpe, S. A., 1992. The generation of internal waves by flow over the rough topography of a continental slope.Proceedings of the Royal Society of London A439: 115–130.

Tyhurst, M. F., 1978. Tidal conditions in Poole Bay.Journal of the Society of Civil Engineering Technicians 5(6): 6–11.

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