极端风力条件下巴拉克拉瓦湾的风浪

V. Fomin, A. Polozok
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引用次数: 0

摘要

海湾和港口的风浪对沿海基础设施的航行和运行安全具有重要影响。本工作的目的是研究不同风况下克里米亚半岛巴拉克拉瓦湾的风浪特征。该研究是在使用一系列嵌套网格的数值谱SWAN波模型的基础上进行的。对巴拉克拉瓦湾的波浪进行了具体的计算,以适应不同方向的持续风和2007年11月黑海出现的极端风暴。研究发现,在海湾的南部,最强烈的波浪是由南风形成的。在海湾入口处,在一年一次和25年一次的风速下,显著波高hs的最大值分别为3 m和5.4 m。在海湾北部,有风的最大值为0.25和0.46 m,分别为一年一次和25年一次。定义风暴波在穿过海湾南部的狭长地带向海湾北部传播时迅速减弱。因此,局地风场是影响巴拉克拉瓦湾北部波浪强度的决定性因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Wind Waves in the Balaklava Bay under Extreme Wind Conditions
Wind waves in bays and harbors have a significant impact on the safety of navigation and operation of the coastal infrastructure. The purpose of this work is to study the characteristics of wind waves in the Balaklava Bay (Crimean Peninsula) under different wind conditions. The study was carried out on the basis of a numerical spectral SWAN wave model using a sequence of nested grids. Specific calculations of waves in the Balaklava Bay are carried out for constant winds of different directions and for an extreme storm emerged in the Black Sea in November 2007. It was found that in the southern part of the bay the most intense waves are formed with southerly winds. At the bay entrance, at wind speeds, which can occur once a year and once every 25 years, the maximum values of the significant wave height hs amount to 3 and 5.4 m, respectively. In the northern part of the bay, the maximum values hs with winds, which can occur once a year and once every 25 years, respectively, are equal to 0.25 and 0.46 m. It was defined that the storm waves penetrating into the southern part of the bay quickly attenuate as they spread through the narrowness to the northern part of the bay. Thus, the local wind field is the determining factor affecting the intensity of waves in the northern part of the Balaklava Bay.
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