库页岛霍尔姆斯克港的海浪特征

A. Borisov
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引用次数: 0

摘要

在港口建设和改造过程中,以计算出的风浪、风暴潮、水域低频振荡等特征为指导。但是,如果不考虑在不同条件下对特定港口的海浪的实地观测,就不可能正确地确定特征。这项工作补充了库页岛主要港口在2007年进行的海平面测量基础上的波浪特征的现有数据。估计了港区海浪的主要特征:海面振荡幅值、波浪能谱的峰值分量和相应的振荡周期。在这种情况下,峰值分量在从风浪到低频地震振荡的周期范围内确定。分析了风暴情况和平静海况。显示了振荡的共振性质。在平静天气下,能谱中的峰值分量集中在500 s对应的港口自然振荡零模区。在风暴最活跃的阶段,峰值分量主要出现在8s周期附近,风暴开始和结束时的峰值分量出现在182s周期附近,对应于自然振荡的第一模态。对大范围周期内的峰谱分量的分析使我们能够追踪港口内海浪的动力学和海啸振荡的形成过程。
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Sea wave characteristics in the port of Kholmsk (Sakhalin Island)
During construction and reconstruction of ports, they are guided by the calculated characteristics of wind waves, storm surges, low-frequency oscillations of water areas (seiches). However, the correct determination of charac­teristics is impossible without taking into account field observations of sea waves in a particular port under different conditions. This work supplements the existing data on wave characteristics in the main port of Sakhalin Island on the basis of sea level measurements carried out in 2007. The main characteristics of sea waves in the port area were estimated: amplitudes of sea surface oscillations, peak components of the wave energy spectrum and the corresponding periods of oscillations. In this case, the peak components were determined in the range of periods from wind waves to low-frequency seiche oscillations. Storm situations and calm sea conditions were analyzed. The resonant nature of oscillations is shown. It has been established that in calm weather the peak components in the energy spectrum are concentrated in the region of the zero mode of natural oscillations in the port corresponding to 500 s. In the most active phase of storms, the peak component manifests itself mainly near the period of 8 s, and at the beginning and end of the storm it is near the period of 182 s, corresponding to the first mode of natural oscillations. The analysis of peak spectral components in a wide range of periods allows us tracing the dynamics of sea waves in the port and the process of build-up of seiche oscillations.
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来源期刊
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7
审稿时长
12 weeks
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