• Title/Summary/Keyword: Sound Speed Profile (SSP)

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Ranging Algorithm of Underwater Acoustic Wave with Look-up Table (Look-up table을 이용한 수중 음향파 거리 추정 알고리즘)

  • Cheon, Ju-Hyun;Moon, Seung-Hyun;Lee, Ho-Kyoung
    • Journal of the Institute of Electronics and Information Engineers
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    • v.52 no.4
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    • pp.23-29
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    • 2015
  • In this paper, we introduce a underwater ranging algorithm with Look-up Table (LUT) by modifying the existing method which is using the changes of angles of accoustic rays with SSP (Sound Speed Profile). We compare the horizontal distance errors and the calculation times. Our new algorithm exploits Time of Arriva l(ToA) - horizontal distance table based on SSP. This algorithm offers faster calculation speed than the previous one with the slight increase of the distance estimation error.

A Study on the Characteristics of Underwater Sound Transmission by Short-term Variation of Sound Speed Profiles in Shallow-Water Channel with Thermocline (수온약층이 존재하는 천해역에서 단기간 음속구조 변화에 따른 음향 신호 전달 변동에 관한 연구)

  • Jeong, Dong-Yeong;Kim, Sea-Moon;Byun, Sung-Hoon;Lim, Yong-Kon
    • The Journal of the Acoustical Society of Korea
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    • v.34 no.1
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    • pp.20-35
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    • 2015
  • Underwater acoustic channel impulse responses (CIR) are influenced by sound speed profile (SSP), and the variation of CIR has significant effects on the performance of underwater acoustic communication systems. A significant change of SSP can occur within a short period, which must be considered during the design of underwater acoustic modems. This paper statistically analyzes the effect of the variation of SSP on the long-range acoustic signal propagation in shallow-water with thermocline using numerical modeling based on the data acquired from JACE13 experiment near Jeju island. The analysis result shows that CIR changes variously according to the SSP and the depth of the transmitter and receiver. We also found that when the transmitter and receiver are deeper, the variation of sound wave propagation pattern is smaller and signal level becomes higher. All CIR obtained in this study show that a series of bottom reflections due to downward refraction and small bottom loss in the shallow water with thermocline can be very important factor for long-range signal transmission and the performance of underwater acoustic communication system in time varying ocean environment can be very sensitive to the variation of SSP even for a short period of time.

Improvement of the accuracy of XBT based underwater sound speed using the unmanned maritime system and satellite remote sensing data in the Yellow Sea (해양무인체계와 위성 원격탐사 자료를 이용한 XBT 기반의 황해 수중음속 정확도 향상 방안)

  • Kil, Bum-Jun
    • The Journal of the Acoustical Society of Korea
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    • v.38 no.6
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    • pp.621-629
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    • 2019
  • A logical measure is suggested to estimate an accurate Sound Speed Profile (SSP) for the unusual variation of salinity in the Yellow Sea. Based on National Aeronautics and Space Administration (NASA)'s Aqua and Soil Moisture Active Passive (SMAP) satellite data, this measure identifies the area of temperature inversion effect and expansion of low salinity (<30.5 psu) water. Subsequently, on the area, the Conductivity, Temperature, and Depth (CTD) mounted unmanned maritime system estimates accurate SSP. In order to carry out this measure conveniently, a flow chart is demonstrated in this research. By using this measure which finds the high variational salinity area, the inaccuracy issue for calculating SSP from Expandable Bathy Thermograph (XBT) is expected to be solved.

3-D Near Field Localization Using Linear Sensor Array in Multipath Environment with Inhomogeneous Sound Speed (비균일 음속 다중경로환경에서 선배열 센서를 이용한 근거리 표적의 3차원 위치추정 기법)

  • Lee Su-Hyoung;Choi Byung-Woong
    • The Journal of the Acoustical Society of Korea
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    • v.25 no.4
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    • pp.184-190
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    • 2006
  • Recently, Lee et al. have proposed an algorithm utilizing the signals from different paths by using bottom mounted simple linear array to estimate 3-D location of oceanic target. But this algorithm assumes that sound velocity is constant along depth of sea. Consequently, serious performance loss is appeared in real oceanic environment that sound speed is changed variously. In this paper, we present a 3-D near field localization algorithm for inhomogeneous sound speed. The proposed algorithm adopt localization function that utilize ray propagation model for multipath environment with linear sound speed profile(SSP), after that, the proposed algorithm searches for the instantaneous azimuth angle, range and depth from the localization cost function. Several simulations using linear SSP and non linear SSP similar to that of real oceans are used to demonstrate the performance of the proposed algorithm. The estimation error in range and depth is decreased by 100m and 50m respectively.

Acoustic Channel Formation and Sound Speed Variation by Low-salinity Water in the Western Sea of Jeju during Summer (여름철 제주 서부해역의 저염분수로 인한 음속변화와 음파채널 형성)

  • Kim, Juho;Bok, Tae-Hoon;Paeng, Dong-Guk;Pang, Ig-Chan;Lee, Chongkil
    • The Journal of the Acoustical Society of Korea
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    • v.32 no.1
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    • pp.1-13
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    • 2013
  • Salinity does not generally affect sound speed because it shows very small variations in the ocean. However, low salinity water appears in the Western Sea of Jeju Island every summer so that sound speed and sound propagation can change near sea surface. We calculated Sound Speed Profile (SSP) using vertical profiles of temperature and salinity, which were averaged over years of normal salinity and low salinity (<28 psu) from 30 years (1980~2009) at 3 sites of Korea Oceanographic Data Center (KODC). As a result, sound speed variation by low salinity alone was -5.36 m/s at sea surface and -1.35 m/s at 10m depth for low salinity environments. Gradient of SSP was positive down to 5 m depth due to decrease of sound speed near surface, leading formation of haline channel. Simulation of acoustic propagation using a ray model (Bellhop) confirmed the haline channel. Haline channel has formed 4 times while hydrostatic channel controlled by only pressure has formed 9 times for 30 years. The haline channel showed larger critical angles of rays than hydrostatic channel. Haline channel was also formed at some sites among 20 measurement sites in low salinity water mass which appeared on August $1^{st}$ 2010.