The paper deals with the role of the vertical flux of turbulent energy in the atmospheric boundary layer. The influence of the divergence of this flux on the vertical wind profile and on the eddy diffusivity is shown by theoretical considerations.
The meridional eddy flux of energy
✍ Scribed by Robert M. White
- Publisher
- John Wiley and Sons
- Year
- 1951
- Tongue
- English
- Weight
- 692 KB
- Volume
- 77
- Category
- Article
- ISSN
- 0035-9009
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✦ Synopsis
Abstract
An investigation of a large number of upper‐air soundings over regions of North America shows that the eddy transport of sensible heat is poleward in the mid‐latitude troposphere, reversing and becoming equatorward in the stratosphere. The eddy transport of sensible heat reaches its maximum in middle latitudes, decreasing both poleward and equatorward. It is shown wherein these results differ from those recently presented by Priestley. The transport of sensible heat has a high seasonal variation, being much stronger in winter than in summer. There are indications that at very low latitudes the eddy sensible‐heat transport is directed equatorward.
The eddy transport of latent energy is described by means of the same soundings and is found to be poleward throughout middle and high latitudes with a maximum at the ground and decreasing with altitude. The principal seasonal variation in the transport of latent energy appears to be the northward shift of the mid‐latitude maximum from winter to summer. This maximum is not very pronounced, the transport in both seasons being relatively constant through middle latitudes.
📜 SIMILAR VOLUMES
## Abstract An assessment is made using simple diffusion theory of the rate of adjustment of profiles and eddy fluxes for (a), the leading‐edge case as a function of distance and (b), the horizontally uniform case as a function of time. The solutions of the appropriate diffusion equations obtained
## Abstract A marked seasonal variation of the poleward angular‐momentum flux for the northern hemisphere in the vicinity of 30°N. latitude is obtained from an analysis of upper‐wind soundings for a period of one year. The angular‐momentum flux appears to be about twice as great during the winter a