INTERNAL WAVE BORE IN THE SHELF ZONE OF THE SEA

被引：10

作者：

Liapidevskii, V. Yu. ^{[1
,2
]}

Novotryasov, V. V. ^{[3
,4
]}

Khrapchenkov, F. F. ^{[3
]}

Yaroshchuk, I. O. ^{[3
]}

机构：

[1] Russian Acad Sci, Siberian Branch, Lavrentev Inst Hydrodynam, Novosibirsk 630090, Russia

[2] Novosibirsk State Univ, Novosibirsk 630090, Russia

[3] Russian Acad Sci, Far Eastern Branch, VI Ilichev Pacific Oceanol Inst, Vladivostok 690041, Russia

[4] Far Eastern Fed Univ, Vladivostok 690041, Russia

来源：

JOURNAL OF APPLIED MECHANICS AND TECHNICAL PHYSICS | 2017年 / 58卷 / 05期

关键词：

stratified flows; solitary waves; internal bore; three-layer shallow water; shelf zone; BREAKING;

D O I：

10.1134/S0021894417050066

中图分类号：

O3 [力学];

学科分类号：

08 ; 0801 ;

摘要：

This paper presents the observation results for the internal wave bore in the coastal region of the Sea of Japan with the use of vertical thermistor chains. The data obtained is interpreted by the mathematical models of shallow water in which the effect of nonlinearity and dispersion on the propagation of internal wave trains is taken into account. Within the framework of the theory of multilayer shallow water, the problem of transformation of a solitary wave into an internal bore is solved, and the possibility of recovery of a space-time picture of the flow during the passage of an internal bore in the section between adjacent experimental bottom stations is demonstrated.

引用

页码：809 / 818

页数：10

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