Local steady circulation observed by moored current-meters at 4000 m depth in the western North Pacific
Author:
Funder
Science and Technology Agency, Japan
Ministry of Education, Science and Culture, Japan
Publisher
Springer Science and Business Media LLC
Subject
Oceanography
Link
http://link.springer.com/content/pdf/10.1007/s10872-019-00522-9.pdf
Reference20 articles.
1. Adcock ST, Marshall DP (2000) Interactions between geostrophic eddies and the mean circulation over large-scale bottom topography. J Phys Oceanogr 30:3223–3228. https://doi.org/10.1175/1520-0485(2000)030%3c3223:IBGEAT%3e2.0.CO;2
2. Amante C, Eakins BW (2009) ETOPO1 1 Arc-Minute Global Relief Model: Procedures, Data Sources and Analysis, NOAA Technical Memorandum NESDIS NGDC-24. National Geophysical Data Center, NOAA. https://doi.org/10.7289/V5C8276M
3. Ambe D, Endoh T, Hibiya T, Imawaki S (2009) Transition to the large meander path of the Kuroshio as observed by satellite altimetry. La mer 47:19–27
4. Beckmann A, Haidvogel DB (1997) A numerical simulation of flow at Fieberling Guyot. J Geophys Res 102:5595–5613
5. Brink KH (1995) Tidal and lower frequency currents above Fieberling Guyot. J Geophys Res 100:10817–10832
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