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    On the Interpretation of Ocean Current Spectra. Part 1: The Kinematics of Three-Dimensional Vector Time Series

    Source: Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 004::page 627
    Author:
    Calman, Jack
    DOI: 10.1175/1520-0485(1978)008<0627:OTIOOC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A general method for representing and interpreting the spectra of three-dimensional vector time series is outlined. Part I contains the formalism for the kinematic interpretation of a single vector time series. Based on the spectrum density matrix, the formalism unifies and extends to three dimensions several descriptions of a vector process. These are the Cartesian, rotary, rotational invariant and hodograph spectrum representations. Empirical modes, which are properties of the measured time series (not of any geometrical or dynamical assumptions) are introduced. These allow independent orthogonal motions at the same frequency to be separated. Finally the notion of a prespecified spectrum, which automatically picks out that part of the measurement which is consistent with all imposed dynamical assumptions. is advanced.
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      On the Interpretation of Ocean Current Spectra. Part 1: The Kinematics of Three-Dimensional Vector Time Series

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    contributor authorCalman, Jack
    date accessioned2017-06-09T14:44:48Z
    date available2017-06-09T14:44:48Z
    date copyright1978/07/01
    date issued1978
    identifier issn0022-3670
    identifier otherams-25827.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162653
    description abstractA general method for representing and interpreting the spectra of three-dimensional vector time series is outlined. Part I contains the formalism for the kinematic interpretation of a single vector time series. Based on the spectrum density matrix, the formalism unifies and extends to three dimensions several descriptions of a vector process. These are the Cartesian, rotary, rotational invariant and hodograph spectrum representations. Empirical modes, which are properties of the measured time series (not of any geometrical or dynamical assumptions) are introduced. These allow independent orthogonal motions at the same frequency to be separated. Finally the notion of a prespecified spectrum, which automatically picks out that part of the measurement which is consistent with all imposed dynamical assumptions. is advanced.
    publisherAmerican Meteorological Society
    titleOn the Interpretation of Ocean Current Spectra. Part 1: The Kinematics of Three-Dimensional Vector Time Series
    typeJournal Paper
    journal volume8
    journal issue4
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1978)008<0627:OTIOOC>2.0.CO;2
    journal fristpage627
    journal lastpage643
    treeJournal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian