Internal marine waves and atmospheric depressions

被引：24

作者：

Dolgikh, G. I. ^{[1
,2
]}

Budrin, S. S. ^{[1
]}

Dolgikh, S. G. ^{[1
]}

Ovcharenko, V. V. ^{[1
]}

Chupin, V. A. ^{[1
]}

Shvets, V. A. ^{[1
]}

Yakovenko, S. V. ^{[1
]}

机构：

[1] Russian Acad Sci, Far East Branch, Ilichev Pacific Oceanol Inst, Vladivostok 690041, Russia

[2] Far Eastern Fed Univ, Sch Nat Sci, Vladivostok, Russia

来源：

DOKLADY EARTH SCIENCES | 2015年 / 462卷 / 02期

基金：

俄罗斯科学基金会;

关键词：

Internal Wave; DOKLADY Earth Science; Propagation Front; Shelf Zone; Crust Layer;

D O I：

10.1134/S1028334X15060112

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

This work describes the results of processing experimental data during synchronous registration of the crust deformations and oscillations of atmospheric and hydrospheric pressures. It was found that internal marine waves with a frequency range from 5 to 20 min are mainly generated by atmospheric disturbances, whose variations are absolutely identical to those of hydrospheric pressure in the shelf zone of the Sea of Japan.

引用

页码：631 / 633

页数：3