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    An Alternate Scale Representation of Atmospheric Energy Spectra

    Source: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 004::page 649
    Author:
    Baer, Ferdinand
    DOI: 10.1175/1520-0469(1972)029<0649:AASROA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Although it is known that all spatial scales are nonlinearly interrelated in any prediction model of the atmosphere, truncation demands a limit to scale resolution. One is therefore compelled to parameterize sub-resolution scales, hopefully in such a manner that they describe observed statistics. Such statistics have been shown frequently as energy spectra of synoptic scales in terms of the planetary wavenumber. An alternate representation is the presentation of the energy in terms of the degree of a Legendre polynomial expansion; this representation may be more advantageous insofar as it presents a two-dimensional spectral index. Arguments are presented which indeed suggest the appropriateness of the index. Two months of atmospheric wind data at five pressure levels and on a hemispheric grid were analyzed to establish energy spectra. The spectra are described both as a function of time and as a function of wavenumber for time averages. Using a five-level linear baroclinic model, stability characteristics for each wave component for the observed zonal and vertical profiles were established. Based on these results, the energy data were fit logarithmically by least squares to the wavenumber (both planetary wavenumber and Legendre polynomial degree). Energy slopes show values close to ?3 when utilizing the two-dimensional index in the non-baroclinically forced scale range. These results suggest the use of this index in studying scale parameterization.
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      An Alternate Scale Representation of Atmospheric Energy Spectra

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    contributor authorBaer, Ferdinand
    date accessioned2017-06-09T14:16:23Z
    date available2017-06-09T14:16:23Z
    date copyright1972/05/01
    date issued1972
    identifier issn0022-4928
    identifier otherams-16164.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151917
    description abstractAlthough it is known that all spatial scales are nonlinearly interrelated in any prediction model of the atmosphere, truncation demands a limit to scale resolution. One is therefore compelled to parameterize sub-resolution scales, hopefully in such a manner that they describe observed statistics. Such statistics have been shown frequently as energy spectra of synoptic scales in terms of the planetary wavenumber. An alternate representation is the presentation of the energy in terms of the degree of a Legendre polynomial expansion; this representation may be more advantageous insofar as it presents a two-dimensional spectral index. Arguments are presented which indeed suggest the appropriateness of the index. Two months of atmospheric wind data at five pressure levels and on a hemispheric grid were analyzed to establish energy spectra. The spectra are described both as a function of time and as a function of wavenumber for time averages. Using a five-level linear baroclinic model, stability characteristics for each wave component for the observed zonal and vertical profiles were established. Based on these results, the energy data were fit logarithmically by least squares to the wavenumber (both planetary wavenumber and Legendre polynomial degree). Energy slopes show values close to ?3 when utilizing the two-dimensional index in the non-baroclinically forced scale range. These results suggest the use of this index in studying scale parameterization.
    publisherAmerican Meteorological Society
    titleAn Alternate Scale Representation of Atmospheric Energy Spectra
    typeJournal Paper
    journal volume29
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1972)029<0649:AASROA>2.0.CO;2
    journal fristpage649
    journal lastpage664
    treeJournal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 004
    contenttypeFulltext
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