Long-Wave Generation due to Atmospheric-Pressure Variation and Harbor Oscillation in Harbors of Various Shapes and Countermeasures against Meteotsunamis

T. Kakinuma
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引用次数: 2

Abstract

First, the generation and propagation of long ocean waves due to the atmospheric-pressure variation have been simulated using the numerical model based on the nonlinear shallow water equations, where the atmospheric-pressure waves of various pressure-profile patterns travel eastward over East China Sea. Before the oscillation attenuation in Urauchi Bay, Japan, the incidence of long waves can continue owing to an oscillation system generated between the main island of Kyushu and Okinawa Trough. Second, the simple estimate equations are proposed to predict both the wave height and wavelength of long waves caused by an atmospheric-pressure wave, using atmospheric-pressure data above the ocean. Third, numerical simulation has been generated for the oscillation in the harbors of C-, I-, L-, and T-type shapes, as well as Urauchi Bay with two bay heads like a T-type harbor. Finally, we discuss disaster measures, including the real-time prediction of meteotsunami generation, as well as both the structural and the nonstructural preparations.
不同形状港口气压变化和港口振荡引起的长波产生及应对气象海啸的对策
首先,利用基于非线性浅水方程的数值模型,模拟了东海上空各种气压剖面型的气压波在东向传播过程中由于气压变化引起的长海浪的产生和传播。在日本浦内湾振荡衰减之前,由于九州本岛与冲绳海槽之间产生振荡系统,长波的发生率可以继续。其次,利用海洋上空的大气压力数据,提出了简单的估算方程来预测由大气压力波引起的长波的波高和波长。第三,对C-型、I-型、L-型、t型四种形状的港湾,以及像t型港湾一样有两个湾头的浦内湾的振荡进行了数值模拟。最后,我们讨论了灾害措施,包括海啸产生的实时预测,以及结构和非结构准备。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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