Abstract
Large-scale vortex structures (atmospheric cyclones and anticyclones, and synoptic vortexes of the open ocean) play a significant role in the formation of weather and climate as well as in the processes of passive scalar transport [1]. An increase in the lifetime of large scale vortexes is possible at mid-latitudes due to the phenomenon of atmospheric blocking [2]. Such eddy formations were found in zonal currents, which exist in the atmospheres of large planets of the Solar System: Jupiter and Saturn. The best known is the Great Red Spot of Jupiter [3]. We can currently distinguish two approaches to the description of large-scale vortex structures in the oceans
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