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    Staggered Turkel-Zwas Schemes for Two-Dimensional Shallow-Water Equations

    Source: Monthly Weather Review:;1994:;volume( 122 ):;issue: 001::page 223
    Author:
    Song, Yuhe
    ,
    Tang, Tao
    DOI: 10.1175/1520-0493(1994)122<0223:STZSFT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The Turkel-Zwas-type schemes employ coarse grids to discretize the terms associated with the fast gravity-inertia waves and use fine grids to treat the terms associated with the slow Rossby waves. The ratio of the coarse and fine grids is an integer, p>1, and one can use time steps nearly p times larger than those allowed by the Courant-Friedrich-Lewy condition for the usual explicit leapfrog scheme. This paper investigates the Turkel-Zwas-type schemes with three spatial grids-namely, A (unstaggered), B, and C grids (staggered)-for two-dimensional shallow-water equations. A new method that uses the Laplace transform is introduced to solve the two-dimensional phase solutions. Comparisons of the three grids with coarse and fine-grid resolutions are made. One realistic model problem is tested to verify the linear analysis results. The test shows that the Turkel-Zwas-type schemes can be used for a larger time step in some practical simulations.
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      Staggered Turkel-Zwas Schemes for Two-Dimensional Shallow-Water Equations

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4203211
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    contributor authorSong, Yuhe
    contributor authorTang, Tao
    date accessioned2017-06-09T16:09:46Z
    date available2017-06-09T16:09:46Z
    date copyright1994/01/01
    date issued1994
    identifier issn0027-0644
    identifier otherams-62331.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203211
    description abstractThe Turkel-Zwas-type schemes employ coarse grids to discretize the terms associated with the fast gravity-inertia waves and use fine grids to treat the terms associated with the slow Rossby waves. The ratio of the coarse and fine grids is an integer, p>1, and one can use time steps nearly p times larger than those allowed by the Courant-Friedrich-Lewy condition for the usual explicit leapfrog scheme. This paper investigates the Turkel-Zwas-type schemes with three spatial grids-namely, A (unstaggered), B, and C grids (staggered)-for two-dimensional shallow-water equations. A new method that uses the Laplace transform is introduced to solve the two-dimensional phase solutions. Comparisons of the three grids with coarse and fine-grid resolutions are made. One realistic model problem is tested to verify the linear analysis results. The test shows that the Turkel-Zwas-type schemes can be used for a larger time step in some practical simulations.
    publisherAmerican Meteorological Society
    titleStaggered Turkel-Zwas Schemes for Two-Dimensional Shallow-Water Equations
    typeJournal Paper
    journal volume122
    journal issue1
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1994)122<0223:STZSFT>2.0.CO;2
    journal fristpage223
    journal lastpage234
    treeMonthly Weather Review:;1994:;volume( 122 ):;issue: 001
    contenttypeFulltext
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    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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