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    An Experimental Study of Baroclinic Annulus Waves at Large Taylor Number

    Source: Journal of the Atmospheric Sciences:;1972:;Volume( 029 ):;issue: 004::page 665
    Author:
    Ketchum, Carl B.
    DOI: 10.1175/1520-0469(1972)029<0665:AESOBA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A detailed survey of the temperature structure of the upper symmetric, regular wave, and irregular regimes in a differentially heated rotating annulus is presented. The results were obtained in a large gap width, b ? a = 15.28 cm, where a and b are the radii of the inner and outer walls of the annulus respectively, using a 4 ? 4 grid of fine wire thermocouples. The principal results are: The value of Θ = gd??/[??Ω(b?a)], where g is the acceleration of gravity, d the depth of the fluid, ?? the density difference corresponding to an impressed temperature difference of ??, ?? the mean density of the fluid and Ω the rotation rate of the annulus, at the transition between the symmetric and regular wave regimes, is 3.7 for values of the Taylor number T = [4Ω(b ? c)4/?][(b ? a)/d] between 2.7 ? 107 < T < 9.8 ? 107, where v? is the mean coefficient of kinematic viscosity of the fluid. The vertical temperature difference within the fluid is almost independent of the rotation rate and flow regime, having a mean value of 0.78?T. The radial temperature difference outside of the side wall boundary layers exhibits more variation with the rotation rate and flow regime. The waves in the regular wave regime are a result of the baroclinic instability of the fluid and bear a qualitative resemblance to the waves obtained in Eady's model using the observed mean wave state to determine the basic state of the model. This latter result is obtained using the numerical results of Williams in conjunction with the experimental observations. The transition from the regular wave regime to the irregular regime occurs at much larger values of T than indicated by previous results using annuli with smaller gap widths and larger aspect ratios [d/(b ? a)].
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      An Experimental Study of Baroclinic Annulus Waves at Large Taylor Number

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4151918
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    • Journal of the Atmospheric Sciences

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    contributor authorKetchum, Carl B.
    date accessioned2017-06-09T14:16:23Z
    date available2017-06-09T14:16:23Z
    date copyright1972/05/01
    date issued1972
    identifier issn0022-4928
    identifier otherams-16165.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151918
    description abstractA detailed survey of the temperature structure of the upper symmetric, regular wave, and irregular regimes in a differentially heated rotating annulus is presented. The results were obtained in a large gap width, b ? a = 15.28 cm, where a and b are the radii of the inner and outer walls of the annulus respectively, using a 4 ? 4 grid of fine wire thermocouples. The principal results are: The value of Θ = gd??/[??Ω(b?a)], where g is the acceleration of gravity, d the depth of the fluid, ?? the density difference corresponding to an impressed temperature difference of ??, ?? the mean density of the fluid and Ω the rotation rate of the annulus, at the transition between the symmetric and regular wave regimes, is 3.7 for values of the Taylor number T = [4Ω(b ? c)4/?][(b ? a)/d] between 2.7 ? 107 < T < 9.8 ? 107, where v? is the mean coefficient of kinematic viscosity of the fluid. The vertical temperature difference within the fluid is almost independent of the rotation rate and flow regime, having a mean value of 0.78?T. The radial temperature difference outside of the side wall boundary layers exhibits more variation with the rotation rate and flow regime. The waves in the regular wave regime are a result of the baroclinic instability of the fluid and bear a qualitative resemblance to the waves obtained in Eady's model using the observed mean wave state to determine the basic state of the model. This latter result is obtained using the numerical results of Williams in conjunction with the experimental observations. The transition from the regular wave regime to the irregular regime occurs at much larger values of T than indicated by previous results using annuli with smaller gap widths and larger aspect ratios [d/(b ? a)].
    publisherAmerican Meteorological Society
    titleAn Experimental Study of Baroclinic Annulus Waves at Large Taylor Number
    typeJournal Paper
    journal volume29
    journal issue4
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1972)029<0665:AESOBA>2.0.CO;2
    journal fristpage665
    journal lastpage679
    treeJournal of the Atmospheric Sciences:;1972:;Volume( 029 ):;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