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    THE CONTRIBUTION OF DIVERGENT WIND COMPONENTS TO THE ENERGY EXCHANGE BETWEEN THE BAROCLINIC AND BAROTROPIC COMPONENTS 

    Source: Monthly Weather Review:;1966:;volume( 094 ):;issue: 001:;page 1
    Author(s): WIIN-NIELSEN, A.; DRAKE, MARGARET
    Publisher: American Meteorological Society
    Abstract: The contribution from the divergent part of the horizontal wind to the energy conversion between the vertical shear flow and the vertical mean flow has been computed using atmospheric data from the isobaric surfaces: 850, ...
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    ON THE ENERGY EXCHANGE BETWEEN THE BAROCLlNlC AND BAROTROPIC COMPONENTS OF ATMOSPHERIC FLOW 

    Source: Monthly Weather Review:;1965:;volume( 093 ):;issue: 002:;page 79
    Author(s): WIIN-NIELSEN, A.; DRAKE, MARGARET
    Publisher: American Meteorological Society
    Abstract: The energy conversion between the vertical shear flow and the vertical mean flow has been computed using atmospheric data from the isobaric surfaces: 850, 700,500, 300, and 200 mb. In comparison with earlier calculations ...
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    AN OBSERVATIONAL STUDY OF KINETIC ENERGY CONVERSIONS IN THE ATMOSPHERE 

    Source: Monthly Weather Review:;1966:;volume( 094 ):;issue: 004:;page 221
    Author(s): WIIN-NIELSEN, A.; DRAKE, MARGARET
    Publisher: American Meteorological Society
    Abstract: The total kinetic energy in the atmosphere has been subdivided into four energy reservoirs. The partition of the kinetic energy is accomplished by dividing the total flow into the vertical mean flow (the barotropic con ...
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