Penetration depth of the dynamic response of seabed induced by internal solitary waves

Author:

Tian Zhuangcai,Chen Tian,Yu Le,Guo Xiujun,Jia Yonggang

Funder

National Natural Science Foundation of China

NSFC-Shandong Joint Found for Marine Science Research Centers

Fundamental Research Funds for the Central Universities

Publisher

Elsevier BV

Subject

Ocean Engineering

Reference49 articles.

1. An extreme internal solitary wave event observed in the northern South China Sea;Huang;Sci. Rep.,2016

2. Laboratory observations on internal solitary wave evolution on steep and inverse uniform slopes;Chen;Ocean. Eng.,2007

3. Very large subaqueous sand dunes on the upper continental slope in the South China Sea generated by episodic, shoaling deep-water internal solitary waves;Reeder;Mar. Geol.,2011

4. Footprints of obliquely incident internal solitary waves and internal tides near the shelf break in the northern South China Sea: FOOTPRINTS OF ISWS AND INTERNAL TIDES;Ma;Journal of Geophysical Research: Oceans,2016

5. Vertical migration of fine-grained sediments from the interior to the surface of seabed driven by seepage flows “sub-bottom sediment pump action”;Zhang;J. Ocean Univ. China (Oceanic and Coastal Sea Research),2017

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