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Saltzman, Barry; Fleisher, Aaron (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Subjects:
The rate of transfer of kinetic energy between the different scales of eddies of the 500 mb geostrophic wind has been measured for each day of 1951. In the mean, there is a net transfer from intermediate (cyclone) scales to both longer and shorter scales.DOI: 10.1111/j.2153-3490.1960.tb01324.x
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    • FJ~RTOFRT.,,1953: On the changes in the spectral distribution of kinetic energy for two-dimensional nondivergent flow. Tellus 5 , pp. 225-230.
    • SALTZMABN., 1957: Equations governing the energetics of the larger scales of atmospheric turbulence in the domain of wave number./. Meteor. 14,pp. 313-523.
    • SALTZMABN.,, 1959: On the maintenance of the largescale quasipermanent disturbances in the atmosphere. Tellus 11, pp. 423-431.
    • SALTZMANB,., and FLEISHERA,., 1959: The modes of release of available potential energy. Sci. Rpt. No. I. M.I.T.Plan. Circ. Proj., AF19(604)-4958, 20 pp. (also,]. Geophys. Res. 6 5 , pp. 121$-1222, 1960).
    • SALTZMANB,., and FLEISHERA,., 1960. Spectrum of kinetic energy transfer due to large-scale horizontal Reynolds stresses. Tellus 12, pp. 110-111.
    • WIIN-NIELSENA,., 1959: A study of energy conversion and meridional circulation for the large-scale motion in the atmosphere. M o . Weath. R e v . 87, pp. 319-332-
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