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- W8739560 abstract "Some general characters of fluid motion in the fields of gravity and Coriolis force are dealt with in this paper. A concept of is proposed. It is proved that under certain conditions this exists, i. e. the motion finally approaches axially symmetric zonal circulation; but under other conditions complete adaptation is impossible, e. g. in the case of several vortex centres there can never be axially symmetric zonal circulation. With the help of the theory of rotational adaptation process, the existence of negative viscosity, the process of energy concentration and the transition from low index circulation to high index circulation in the atmosphere can be explained. Morcover, it is indicated that high level intonsive vortex centres and surface advective regions and their relative arrangement are the decisive factors in the medium and long-range evolution process of weather systems. The exchange of energy between the motions of various scales is also discussed, and it is concluded that Fjortoft's results can not be applied directly, and the motion of rotating atmosphere is not isotropic." @default.
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- W8739560 date "1979-01-01" @default.
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- W8739560 title "ON NONLINEAR INTERACTION OF MOTION AND PROCESS OF ROTATIONAL ADAPTATION IN ROTATING ATMOSPHERE" @default.
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