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Characteristics of Ocean Wave Radiation Patterns in a Dense Layer of Fluid

밀도층 유체에서 해양 방사파 패턴 특징

  • Min, Eun-Hong (Department of Naval Architecture and Ocean Engineering, Inha University) ;
  • Choi, Ha-Yun (Department of Naval Architecture and Ocean Engineering, Inha University) ;
  • Kim, Young-Gyu (Agency for Defense Development) ;
  • Paik, Kwang-Jun (Department of Naval Architecture and Ocean Engineering, Inha University) ;
  • Koo, Weon-Cheol (Department of Naval Architecture and Ocean Engineering, Inha University)
  • 민은홍 (인하대학교 조선해양공학과) ;
  • 최하윤 (인하대학교 조선해양공학과) ;
  • 김영규 (국방과학연구소) ;
  • 백광준 (인하대학교 조선해양공학과) ;
  • 구원철 (인하대학교 조선해양공학과)
  • Received : 2018.10.08
  • Accepted : 2019.02.22
  • Published : 2019.02.28

Abstract

The sea is stratified with water that has different densities because of pressure, temperature, and salinity. When conducting studies of internal waves in the ocean, the fluid is assumed to have layers that have discrete densities. This assumption is made because it is difficult to achieve layers that exhibit gradual changes in the density of the water. In this study, we used previous studies on ocean waves and their radiation issues in the density layer fluid to investigate the characteristics of internal waves in the ocean and their radiation patterns induced by a moving body in a stratified fluid. We also studied the difference in wave radiation between the density gradient layer and the discrete density layer. We found that the wave radiation patterns depended on the velocity of the moving body and the change in the density of the water. The crest apex shift phenomenon was observed in the density gradient in the layer of fluid.

Keywords

Brunt-$V{\ddot{a}}is{\ddot{a}}l{\ddot{a}}$ frequency;Internal wave;Stratification;Density gradient layer;Discrete density layer

Acknowledgement

Supported by : 국방과학연구소, 한국연구재단

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