Influence of the Cape Angle and Flow Speed on Eddy Formation and Detachment: Experimental Results and Comparison with North Brazil Current Eddies
Author:
Publisher
Springer Science and Business Media LLC
Subject
Oceanography
Link
https://link.springer.com/content/pdf/10.1007/s12601-022-00087-7.pdf
Reference32 articles.
1. Aroucha LC, Veleda D, Lopes FS, Tyaquiçã P, Lefèvre N, Araujo M (2020) Intra-and inter-annual variability of North Brazil Current rings using angular momentum eddy detection and tracking algorithm: observations from 1993 to 2016. J Geophys Res Oceans 125:e2019JC015921. https://doi.org/10.1029/2019JC015921
2. Avicola G, Huq P (2002) Scaling analysis for the interaction between a buoyant coastal current and the continental shelf: experiments and observations. J Phys Oceanogr 32:3233–3248. https://doi.org/10.1175/1520-0485(2002)032<3233:SAFTIB>2.0.CO;2
3. Avicola G, Huq P (2003) The role of outflow geometry in the formation of the recirculating bulge region in coastal buoyant outflows. J Mar Res 61:411–434. https://doi.org/10.1357/002224003322384870
4. Castelão GP, Johns WE (2011) Sea surface structure of North Brazil Current rings derived from shipboard and moored acoustic Doppler current profiler observations. J Geophys Res Oceans 116:C01010. https://doi.org/10.1029/2010JC006575
5. Cenedese C, Whitehead JA (2000) Eddy shedding from a boundary current around a cape over a sloping bottom. J Phys Oceanogr 30:1515–1531. https://doi.org/10.1175/1520-0485(2000)030<1514:ESFABC>2.0.CO;2
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