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    On the Steady-State Energy Balance of Short Gravity Wave Systems

    Source: Journal of Physical Oceanography:;1980:;Volume( 010 ):;issue: 009::page 1340
    Author:
    Plant, William J.
    DOI: 10.1175/1520-0485(1980)010<1340:OTSSEB>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Steady-state energy balances of short gravity wave systems generated in a wave tank with and without airflow have been measured and compared with the predictions of perturbation theory. Wind-wave spectra were found to fit a JONSWAP form to a good approximation if a wind-dependent equilibrium range coefficient was used. Mechanically generated waves were produced which had frequency spectra similar to wind-generated wave spectra and which exhibited nonlinear effects through a decrease in the spectral peak frequency with fetch. In the wind-wave case, perturbation theory well predicted the difference between the net source function and energy input from the wind for a wide range of fetch and wind speed conditions provided that surface tension was properly taken into account. In the case of waves generated without airflow, perturbation theory predicted energy transfer rates much smaller than the measured values.
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      On the Steady-State Energy Balance of Short Gravity Wave Systems

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162981
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    contributor authorPlant, William J.
    date accessioned2017-06-09T14:45:34Z
    date available2017-06-09T14:45:34Z
    date copyright1980/09/01
    date issued1980
    identifier issn0022-3670
    identifier otherams-26121.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162981
    description abstractSteady-state energy balances of short gravity wave systems generated in a wave tank with and without airflow have been measured and compared with the predictions of perturbation theory. Wind-wave spectra were found to fit a JONSWAP form to a good approximation if a wind-dependent equilibrium range coefficient was used. Mechanically generated waves were produced which had frequency spectra similar to wind-generated wave spectra and which exhibited nonlinear effects through a decrease in the spectral peak frequency with fetch. In the wind-wave case, perturbation theory well predicted the difference between the net source function and energy input from the wind for a wide range of fetch and wind speed conditions provided that surface tension was properly taken into account. In the case of waves generated without airflow, perturbation theory predicted energy transfer rates much smaller than the measured values.
    publisherAmerican Meteorological Society
    titleOn the Steady-State Energy Balance of Short Gravity Wave Systems
    typeJournal Paper
    journal volume10
    journal issue9
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1980)010<1340:OTSSEB>2.0.CO;2
    journal fristpage1340
    journal lastpage1352
    treeJournal of Physical Oceanography:;1980:;Volume( 010 ):;issue: 009
    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
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