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    A “Vertically Lagrangian” Finite-Volume Dynamical Core for Global Models

    Source: Monthly Weather Review:;2004:;volume( 132 ):;issue: 010::page 2293
    Author:
    Lin, Shian-Jiann
    DOI: 10.1175/1520-0493(2004)132<2293:AVLFDC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A finite-volume dynamical core with a terrain-following Lagrangian control-volume discretization is described. The vertically Lagrangian discretization reduces the dimensionality of the physical problem from three to two with the resulting dynamical system closely resembling that of the shallow water system. The 2D horizontal-to-Lagrangian-surface transport and dynamical processes are then discretized using the genuinely conservative flux-form semi-Lagrangian algorithm. Time marching is split-explicit, with large time steps for scalar transport, and small fractional steps for the Lagrangian dynamics, which permits the accurate propagation of fast waves. A mass, momentum, and total energy conserving algorithm is developed for remapping the state variables periodically from the floating Lagrangian control-volume to an Eulerian terrain-following coordinate for dealing with ?physical parameterizations? and to prevent severe distortion of the Lagrangian surfaces. Deterministic baroclinic wave-growth tests and long-term integrations using the Held?Suarez forcing are presented. Impact of the monotonicity constraint is discussed.
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      A “Vertically Lagrangian” Finite-Volume Dynamical Core for Global Models

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4205447
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    contributor authorLin, Shian-Jiann
    date accessioned2017-06-09T16:15:39Z
    date available2017-06-09T16:15:39Z
    date copyright2004/10/01
    date issued2004
    identifier issn0027-0644
    identifier otherams-64343.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4205447
    description abstractA finite-volume dynamical core with a terrain-following Lagrangian control-volume discretization is described. The vertically Lagrangian discretization reduces the dimensionality of the physical problem from three to two with the resulting dynamical system closely resembling that of the shallow water system. The 2D horizontal-to-Lagrangian-surface transport and dynamical processes are then discretized using the genuinely conservative flux-form semi-Lagrangian algorithm. Time marching is split-explicit, with large time steps for scalar transport, and small fractional steps for the Lagrangian dynamics, which permits the accurate propagation of fast waves. A mass, momentum, and total energy conserving algorithm is developed for remapping the state variables periodically from the floating Lagrangian control-volume to an Eulerian terrain-following coordinate for dealing with ?physical parameterizations? and to prevent severe distortion of the Lagrangian surfaces. Deterministic baroclinic wave-growth tests and long-term integrations using the Held?Suarez forcing are presented. Impact of the monotonicity constraint is discussed.
    publisherAmerican Meteorological Society
    titleA “Vertically Lagrangian” Finite-Volume Dynamical Core for Global Models
    typeJournal Paper
    journal volume132
    journal issue10
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(2004)132<2293:AVLFDC>2.0.CO;2
    journal fristpage2293
    journal lastpage2307
    treeMonthly Weather Review:;2004:;volume( 132 ):;issue: 010
    contenttypeFulltext
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