References
1. Alekseev, G. V., Bagryantsev, M. V., Bogorodskiy, P. V., Vasin, V. V., & Shirokov, P. E.
(1991). Structure and circulation of water in the area of anticyclonic eddy in the northeastern
Norwegian Sea. Problems of the Arctic and Antarctic, 65, 14–23 (in Russian).
2. Alekseev, G. V., Nikolaev, Yu V, Romanov, A. A., Romantsev, V. A., & Sarukhanyan, E. I.
(1986). Results of natural investigations in the Norwegian energy active zone. Itogi Nauki i
Tekhniki, Atmosphere, Ocean, Space Program RAZREZY, 7, 46–72 (in Russian).
3. Argo. (2000). Argo float data and metadata from Global Data Assembly Center (Argo
GDAC). SEANOE. http://doi.org/10.17882/42182.
4. Bashmachnikov, I. L., Sokolovskiy, M. A., Belonenko, T. V., Volkov, D. L., Isachsen, P. E.,
& Carton, X. (2017). On the vertical structure and stability of the Lofoten vortex in the
Norwegian Sea. Deep-Sea Research Part I (in press).
5. Gascard, J.-C., & Mork, K. A. (2008). Climatic importance of large-scale and mesoscale
circulation in the Lofoten Basin deduced from Lagrangian observations. In R. R. Dickson,
J. Meincke, & P. Rhines (Eds.), Chapter 6: Arctic-Subarctic Ocean fluxes. Defining the role
of the Northern Seas in climate (pp. 131–143). Dordrecht: Springer.
6. Ivanov, V. V., & Korablev, A. A. (1995). Formation and regeneration of the pycnocline lens
in the Norwegian Sea. Russian Meteorology and Hydrology, 9, 62–69.
7. Ivanov, V. V., & Korablev, A. A. (1995). Interpycnocline lens dynamics in the Norwegian
Sea. Russian Meteorology and Hydrology, 10, 32–37.
8. Köhl, A. (2007). Generation and stability of a quasi-permanent vortex in the Lofoten Basin.
Journal of Physical Oceanography, 37, 2637–2651.
9. Kozlov, V. F. (1984). Models of the topographic vortices in ocean (p. 200). Moscow: Nauka.
10. Lebedev, K. V. (2016). An argo-based model for investigation of the Global Ocean
(AMIGO). Oceanology, 56, 172–181.
11. Moshonkin, S. N., Bagno, A. V., Gusev, A. V., Filyushkin, B. N., & Zalesny, V. B. (2017).
Physical properties of the Atlantic-Arctic water exchange formation. Izvestiya Atmospheric
and Oceanic Physics, 53, 213–223.
12. Orvik, K. A. (2004). The deepening of the Atlantic water in the Lofoten Basin of the
Norwegian Sea, demonstrated by using an active reduced gravity model. Geophysical
Research Letters, 31, L01306. https://doi.org/10.1029/2003GL018687.
13. Orvik, K. A., & Niiler, P. (2002). Major pathways of Atlantic water in the northern North
Atlantic and Nordic Seas toward Arctic. Geophysical Research Letters, 29. https://doi.org/10.
1029/2002GL015002.
14. Poulain, P.-M., Warn-Varnas, A., & Niiler, P. P. (1996). Near-surface circulation of the
Nordic Seas as measured by Lagrangian drifters. Journal Geophysical Research, 101, 18237–
18258.
15. Raj, R. P., Chafik, L., Nilsen, J. E. Ø., Eldevik, T., & Halo, I. (2015). The Lofoten Vortex of
the Nordic Seas. Deep-Sea Research Part I, 96, 1–14.
16. Raj, R. P., & Halo, I. (2016). Monitoring the mesoscale eddies of the Lofoten Basin:
Importance, progress, and challenges. International Journal of Remote Sensing, 37, 3712–
3728.
17. Rodionov, V. B., & Kostianoy, A. G. (1998). Oceanic fronts of the North-European basin
seas (293 pp.). Moscow: GEOS (in Russian).
18. Rossby, T., Ozhigin, V., Ivshin, V., & Bacon, Sh. (2009). An isopycnal view of the Nordic
Seas hydrography with focus on properties of the Lofoten Basin. Deep-Sea Research Part I,
56, 1955–1971.
19. Søiland, H., & Rossby, T. (2013). On the structure of the Lofoten Basin Eddy. Journal of
Geophysical Research: Oceans, 118, 4201–4212.
20. Sokolovskiy, M. A. (1991). Modeling triple-layer vortical motions in the ocean by the
Contour Dynamics Method. Izvestiya Atmospheric and Oceanic Physics, 27, 380–388.
346
B. N. Filyushkin et al.
Précédent

- 343/610

Suivant