Energy of the Jets of the Antarctic Circumpolar Current and of Their Eddies in the Surface Layer of the Southern Ocean

Author:

Koshlyakov M. N.,Savchenko D. S.,Tarakanov R. Yu.

Publisher

Pleiades Publishing Ltd

Subject

Oceanography

Reference8 articles.

1. Baroclinic instability of large-scale currents;V. M. Kamenkovich,1987

2. A.G. Kostyanoy, A.I. Ginzburg, S.A. Lebedev et al. “Fronts and Mesoscale Variability in the Southern Indian Ocean as Inferred from the TOPEX/POSEIDON and ERS-2 Altimetry Data”, Oceanology (Engl. Transl.) 43, 632–642 (2003)

3. M. N. Koshlyakov, D. S. Savchenko, and R. Yu. Tarakanov, “Energy exchange between jets of the Antarctic Circumpolar Current and synoptic eddies in the Drake Passage and Scotia Sea,” Oceanology (Engl. Transl.) 58, 329–339 (2018).

4. R. Yu. Tarakanov and A. M. Gritsenko, “The frontal and jet structure south of Africa based on the data of the SR02 section in December of 2009,” Oceanology (Engl. Transl.) 54, 401–413 (2014).

5. R. Yu. Tarakanov and A. M. Gritsenko, “Fine-jet structure of the Antarctic Circumpolar Current south of Africa,” Oceanology (Engl. Transl.) 54, 677–687 (2014).

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