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Sims, Joseph E. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
The mean zonal kinetic energy transports across arbitrary latitude walls in the northern hemisphere are evaluated from five years of data. It is found that the stress-work processes at the boundaries are much more significant than the actual advection of zonal kinetic energy. The stress component associated with the earth's rotation accounts for a net northward transport of zonal kinetic energy across the equator.DOI: 10.1111/j.2153-3490.1970.tb00534.x
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    • Macdonald, N. J. & Frazier, H. M. 1969. A note on the seasonal variation of the flux of angular momentum by transient and standing eddies in the northern hemisphere. Tellus 21, 65C667.
    • Sims, J. E. 1969. Evaluation of the symmetrical zonal kinetic energy equation. MS thesis, MIT. 84 PP.
    • Starr, V. P. & Gaut, N. E. 1969. Symmetrical formulation of the zonal kinetic energy equation. Tellus 21, 185-191.
    • Starr, V. P. & Sims, J. E. 1970. Transport of mean zonal kinetic energy in the atmosphere. Tellus 22, 167-171.
    • Starr, V. P., Peixoto, J. P. & Gaut, N. E. 1970. Momentum and zonal kinetic energy balance of the atmosphere from five years of hemispheric data. Tellus 22, 251-274.
    • Starr, V. P., Peixoto, J. P. & Sims, J. E. 1970. A method for the study of the zonal kinetic energy balance in the atmosphere. Geofis. pur. q p l . In press.
    • Walker, H. C. 1970. Unbiased station grid for study of the kinetic energy balance of the atmosphere. Geofis. pur. appl. I n press.
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