Numerical Simulation of Gravity Waves Excited in the Ocean by Low-Frequency Surface Seismic Waves Based on GPS Recordings


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

详细

A numerical experiment for reproducing the generation of free gravity waves in the ocean by low-frequency surface seismic waves passing across the bottom is described. The dynamics of the bottom movement is reconstructed based on the real GPS data recorded during the disastrous Tohoku earthquake of March 11, 2011. Results of the numerical simulation show that horizontal movements of underwater slopes play a key role in the generation of free gravity waves.

作者简介

K. Sementsov

Department of Physics

编辑信件的主要联系方式.
Email: sebbest@yandex.ru
俄罗斯联邦, Moscow, 119991

M. Nosov

Department of Physics; Institute of Marine Geology and Geophysics, Far Eastern Branch

Email: sebbest@yandex.ru
俄罗斯联邦, Moscow, 119991; Yuzhno-Sakhalinsk, 693022

S. Kolesov

Department of Physics

Email: sebbest@yandex.ru
俄罗斯联邦, Moscow, 119991

Y. Wu

Earthquake Research Institute

Email: sebbest@yandex.ru
日本, 1-1-1 Yayoi, Bunkyo-ku, Tokyo, 113-0032

补充文件

附件文件
动作
1. JATS XML

版权所有 © Allerton Press, Inc., 2017