• Title/Summary/Keyword: atiltness

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Experimental Study for Evaluation of Non-Linear Dispersive Wave Model in Shallow Water (천해역 비선형분산파랑 모델의 평가를 위한 수리 실험 연구)

  • 이중우;신승호
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.11 no.4
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    • pp.189-196
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    • 1999
  • In order to verify a numerical model for the calculation of wave motion around an offshore barrier in shallow water, laboratory physical experiments are necessary. In this study, sample experiments are carried out on the wave and wave induced current fields due to a sloping bottom topography and on that due to an isolated structure from the coastline. The water body is divided into 4 levels, in which the current tracking floaters are deployed to measure the wave induced currents. Data measurement was continued using the limited wave gauges and current tracking floaters including a video camera from the top. The wave heights for the preselected surface and time-averaged velocity distributions at each level were measured in detail. The distribution of wave and current fields was analyzed precisely combining the whole measured laboratory data. Moreover, comprehensive analyses were carried out on non-linearity of wave transformation in terms of skewness and atiltness.

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Wave Data Analysis for Investigation of Freak wave Characteristics (Freak Wave 특성 파악을 위한 파랑관측 자료의 분석)

  • Shin, Seung-Ho;Hong, Key-Yong;Moon, Jae-Seung
    • Journal of Navigation and Port Research
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    • v.31 no.6
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    • pp.471-478
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    • 2007
  • This study is carried out the investigation of nonlinear characteristics of the field wave observation data acquired in the western sea area in Jeju island during one year. It is aimed to offer the fundamental data for Freak wave forecasting in real sea. For this, the nonlinear parameters of ocean waves, which are Skewness, Atiltness, Kurtosis and Spectrum band width parameter et al., are introduced, and the parameters are compared and discussed with some characteristics wave components, ie, significant wave height, maximum wave height, and so on. As a results, we know that the parameters describe nonlinear characteristics of observed wave spectrum broadly, are feebly related with occurrence of abnormal maximum wave height, namely freak event, however the Kurtosis, $K_t$ which is a degree of peakness of mode of surface elevation distribution, has better relationship than others.

Study on Freak Wave Characteristics and Approximation of Wave Spectrum in Uljin Sea Area (울진해역의 Freak wave 특성과 스펙트럼 근사에 대한 연구)

  • Ryu, Hwang-Jin;Hong, Sa-Young
    • Journal of Ocean Engineering and Technology
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    • v.26 no.2
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    • pp.8-13
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    • 2012
  • This paper investigates the statistical properties of waves in the sea area of Uljin, which is located in the East Sea area of Korea. The wave data were measured using AWAC (Acoustic Wave and Current Meter), which was installed at a 16-m water depth from November 2010 to March 2011. The wave data acquisition rate, Hmax, monthly mean Hs, Tz, Tp, and wave direction are summarized. The distributions of Hs and Tz were analyzed using the Hs-Tz scatter diagrams. The measurement wave data were analyzed to investigate freak wave characteristics. By comparing the wave spectrum using the measurement wave data with the wave spectrum obtained by varying the JONSWAP wave spectrum, it was possible to approximate the wave spectrum shape at the Uljin Sea area.

Field Wave Data Analysis for Investigation of Freak wave Characteristics (Freak wave 특성 파악을 위한 파랑관측 자료의 분석)

  • Shin, Seung-Ho;Hong, Key-Yong;Moon, Jae-Seung
    • Proceedings of the Korean Institute of Navigation and Port Research Conference
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    • v.1
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    • pp.175-180
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    • 2006
  • This study is carried out the investigation of nonlinear characteristics of the ocean based on the field wave observation data acquired the western sea area in Jeju island during one year. It is aimed to offer the fundamental data for Freak wave forecasting in real sea. For this, the nonlinearity parameters of ocean waves, which are Skewness, Atiltness, Kurtosis and Spectrum band width parameter, are introduced, and the parameters are compared and discussed with some characteristic wave components, ie, significant wave height, maximum wave height, and so on.

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