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pro vyhledávání: '"D. R. Shvartsman"'
Publikováno v:
Journal of Oceanological Research. :5-35
In this work, by means of laboratory modeling, the patterns of evolution (baroclinic instability and/or viscous degeneration) of mesoscale non-frontal baroclinic eddies, or open ocean eddies (without a core with the water of different density) were r