Observed Taylor cap around a seamount intensified by a surface mesoscale eddy in the Northwest Pacific-Reference-Cited by-同舟云学术

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Observed Taylor cap around a seamount intensified by a surface mesoscale eddy in the Northwest Pacific

Published:2022-12-09 Issue: Volume: Page:
ISSN:0930-7575
Container-title:Climate Dynamics
language:en
Short-container-title:Clim Dyn

Author:

Liu Yansong,Ren Qiang,Yu Fei^ORCID,Wang Jianfeng,Wang Ran,Nan Feng,Ding Yanan,Zheng Tongtong,Zhang Chuanzheng,Zhao Ruixiang,Zheng Hua,Zhu Xiao-Hua

Funder

Natural Science Foundation of Shandong Province

National Natural Science Foundation of China-Shandong Joint Fund for Marine Science Research Centers

the National Key R&D Program of China

National Natural Science Foundation of China

Publisher

Springer Science and Business Media LLC

Subject

Atmospheric Science

Link

https://link.springer.com/content/pdf/10.1007/s00382-022-06570-0.pdf

Reference41 articles.

1. Bashmachnikov I, Loureiro C, Martins A (2013) Topographically induced circulation patterns and mixing over Condor seamount. Deep Sea Res II 98:38–51

2. Beckman A, Haidvogel DB (1997) Numerical simulation of flow at Fieberling Guyot. J Geophys Res 102:5595–5613

3. Brink KH (1990) On the generation of seamount-trapped waves. Deep Sea Res Part I-Oceanograp Res Pap 37(10):1569–1582

4. Brink KH (1995) Tidal and lower frequency currents above Fieberling Guyot. J Geophys Res 100(C6):10817–10832

5. Chapman DC, Haidvogel DB (1992) Formation of Taylor caps over a tall isolated seamount in a stratified ocean. Geophys Astrophys Fluid Dyn 64:31–65

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