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    On the Dynamic Forcing of the Long-Term Mean Flow by the Large-Scale Reynolds' Stresses in the Atmosphere 

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 009:;page 1596
    Author(s): Holopainen, E. O.
    Publisher: American Meteorological Society
    Abstract: Two sets of independent, upper air wind statistical data for the Northern Hemisphere (covering the periods 1950?54 and 1958?62) have been used to make a diagnostic study of some dynamic effects of the transient fluctuations ...
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    Mean Surface Stress Curl over the Oceans as Determined from the vorticity Budget of the Atmosphere 

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 002:;page 262
    Author(s): Holopainen, E. O.; Oort, A. H.
    Publisher: American Meteorological Society
    Abstract: The vertically integrated atmospheric vorticity budget over the oceans offers, in principle, a possibility of determining the surface stress curl from upper wind data without the need to specify a relationship between the ...
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    On the Role of Large-Scale Transient Eddies in the Maintenance of the Vorticity and Enstrophy of the Time-Mean Atmospheric Flow 

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 002:;page 270
    Author(s): Holopainen, E. O.; Oort, A. H.
    Publisher: American Meteorological Society
    Abstract: The global distribution of the forcing of the time-mean flow due to large-scale, horizontal Reynolds stresses (u? u?, v? v?, u? v?) is determined from upper wind statistics for the period 1968?73. The role of this forcing ...
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