Titlebook: Synoptic Eddies in the Ocean; V. M. Kamenkovich,M. N. Koshlyakov,A. S. Monin Book 1986 D. Reidel Publishing Company, Dordrecht, Holland 19

弯腰

companion

摇晃

Stratification and Circulation of the Ocean,cs of sea water. Among such properties and characteristics are the space occupied by sea water in the gravity field (sea level), its phase state (ice cover), the basic thermodynamic characteristics reflecting the state of the water (pressure, temperature, and salinity), derived thermodynamic charact

整顿

organism

缺乏

Eddies in the Open Ocean,n the rest of the ocean? Do formations which in some way resemble eddies of western boundary currents exist in the open ocean? The final answer to this question was given in 1970 by the Soviet expedition ‘Polygon-70’. However, convincing indications of the existence of strong large-scale and long-pe

宣传

Applied Problems,es they produced. The intensity of a disturbance can be defined as the difference δT. between the temperature of the surface water layer in the eddy and the temperature of the surrounding water. Temperature disturbances result in disturbances in the fields of energy fluxes between the sea surface an

ALTER

Stratification and Circulation of the Ocean,eristics (density, electrical conductivity, speed of sound, refractive index, and entropy), the concentration of dissolved gases, bubbles, and organic and mineral suspended matter. Finally, they include characteristics of motion (velocity components and the sea surface level).

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