Bottom Ekman transport drives transverse flows to shape contourite moat and drift systems-Reference-Cited by-同舟云学术

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Bottom Ekman transport drives transverse flows to shape contourite moat and drift systems

Published:2024-10 Issue: Volume:643 Page:118926
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Yin Shaoru^ORCID,Hernández-Molina F. Javier,Mejías Miguel Bruno,Zhao Yulong^ORCID,Manley Tom,Manley Patricia L.,Li Jiabiao

Funder

National Natural Science Foundation of China

Tongji University

National Key Research and Development Program of China

State Key Laboratory of Marine Geology

National Key Research and Development Program of China Stem Cell and Translational Research

Publisher

Elsevier BV

Reference56 articles.

1. A study of the bottom boundary layer over the eastward scarp of the Bermuda Rise;Bird;J. Geophys. Res. Oceans,1982

2. Ten-month observation of the bottom current regime across a sediment drift of the Pacific margin of the Antarctic Peninsula;Camerlenghi;Antarct. Sci.,1997

3. A comparative study of sediment waves and cyclic steps based on geometries, internal structures and numerical modeling;Cartigny;Mar. Geol.,2011

4. Island Wakes in Shallow Water;Dong;Atmosphere-Ocean,2018

5. Controls on upstream-migrating bed forms in sandy submarine channels;Englert;Geology,2023

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