• Title/Summary/Keyword: Minimum Sound Speed Layer

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Variation of Sound Speed in the Tsushima Warm Current Region of the East Sea (동해의 쓰시마난류 분포역에서 음속의 변동)

  • LEE Chung Il;CHO Kyu Dae;KIM Sang Woo
    • Korean Journal of Fisheries and Aquatic Sciences
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    • v.36 no.2
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    • pp.170-177
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    • 2003
  • This study is to analyze the influence of the Tsushima Warm Current (TWC) on the variation of sound speed in the southern part of the East Sea. Sound speed is calculated by method of Chen and Millero (1977:, based on the CTD data measured in June of 1996. Sound speed in the central part of the TWC is about $45ms^{-1}$ more fast than that in the other regions without the TWC. Sound speed minimum layer (SML) in the TWC region exists between loom and 341 m, while it exists between 260m and 290m in the non-TWC region. SML distributes along the path of TWC over continental shelf in the coastal waters of Japan.

Variability of Underwater Sound Propagation in the Northern Part of the East Sea (동해 북부해역의 수중음파전달 변동성)

  • Lim, Se-Han;Yun, Jae-Yul;Kim, Yun-Bae;Nam, Sung-Hyun
    • Journal of the Korea Institute of Military Science and Technology
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    • v.10 no.4
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    • pp.52-61
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    • 2007
  • Temporal and spatial variations of sea water largely affect on the pattern of underwater sound propagation. Acoustic environmental changes and their effects on underwater sound propagation in the northern part of the East Sea, which have been poorly studied mainly due to lack of observations, are investigated by analyzing the hydrographic data acquired since 1993. Severe changes in acoustic environments are associated with various physical processes such as deep convection, thermal fronts, and eddies in the northern part of the East Sea. Spatio-temporal variations of sound speed field and the layer of the maximum sound speed are categorized into six typical cases. Using a sound source of 5 kHz, acoustic transmission losses are calculated range-independently for the six typical cases. Significant differences among the patterns of transmission loss in the six cases suggest that a different tactics are required when we operate in the northern part of the East Sea.

Possibility of False Target Signals Induced by Reverberation Due to Internal Waves in Shallow Water (천해에서 내부파로 인해 생성되는 잔향음에 의한 허위표적 신호 발생 가능성)

  • Lee, Sung Chun;Kim, Sunhyo;Choi, Jee Woong;Kang, Donhyug;Park, Joung Soo;Park, Kyeongju
    • The Journal of the Acoustical Society of Korea
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    • v.34 no.2
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    • pp.98-107
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    • 2015
  • It is investigated that there exists the possibility of the false target signals induced by reverberation in an active sonar system due to the internal waves in shallow water. The rays down-refracted from the internal waves may generate strong bottom-reverberation signals, which can result in false target signals. Sound waves emitted from a source propagate 3-dimensionally. Therefore, the study of internal waves on the reverberation should be studied for azimuthal direction as well as 2-dimensional (r-z) plane. Internal-wave modelling was conducted, based on solitons which were predicted with the various conditions such as, the range of source-soliton, horizontal widths of soliton. Variable depth sonar (VDS) was assumed as a source, of which the depth was located in the minimum sound speed layer in a simulation environment. Finally, the simulation on the reverberation level with time was made based on ray-based reverberation model, and the results implied that several false-target signals could be displayed on the PPI(Plan Position Indicator) scope simultaneously with range from source to soliton, and the horizontal width of soliton.