Abstract
A gas in solid rotation that is subjected to a radial temperature gradient develops a component of heat diffusion at right angles to the gradient. The magnitude of this diffusive flux, relative to the radial component, is 2λΩ/v-, where λ and v- are the mean free path and the mean radial speed of the molecules, respectively, and ω is the angular velocity of the system. Corresponding effects occur in diffusion of mass and momentum. It is suggested that the same effect becomes important in the large-scale turbulent transports in the atmosphere and the oceans. The prediction is that a general eastward eddy heat flux should occur.
© 1966 Pierre Welander, published by Stockholm University Press
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