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    Exploring a Multiresolution Approach Using AMIP Simulations

    Source: Journal of Climate:;2015:;volume( 028 ):;issue: 014::page 5549
    Author:
    Sakaguchi, Koichi
    ,
    Leung, L. Ruby
    ,
    Zhao, Chun
    ,
    Yang, Qing
    ,
    Lu, Jian
    ,
    Hagos, Samson
    ,
    Rauscher, Sara A.
    ,
    Dong, Li
    ,
    Ringler, Todd D.
    ,
    Lauritzen, Peter H.
    DOI: 10.1175/JCLI-D-14-00729.1
    Publisher: American Meteorological Society
    Abstract: his study presents a diagnosis of a multiresolution approach using the Model for Prediction Across Scales?Atmosphere (MPAS-A) for simulating regional climate. Four Atmospheric Model Intercomparison Project (AMIP) experiments were conducted for 1999?2009. In the first two experiments, MPAS-A was configured using global quasi-uniform grids at 120- and 30-km grid spacing. In the other two experiments, MPAS-A was configured using variable-resolution (VR) mesh with local refinement at 30 km over North America and South America and embedded in a quasi-uniform domain at 120 km elsewhere. Precipitation and related fields in the four simulations are examined to determine how well the VRs reproduce the features simulated by the globally high-resolution model in the refined domain. In previous analyses of idealized aquaplanet simulations, characteristics of the global high-resolution simulation in moist processes developed only near the boundary of the refined region. In contrast, AMIP simulations with VR grids can reproduce high-resolution characteristics across the refined domain, particularly in South America. This finding indicates the importance of finely resolved lower boundary forcings such as topography and surface heterogeneity for regional climate and demonstrates the ability of the MPAS-A VR to replicate the large-scale moisture transport as simulated in the quasi-uniform high-resolution model. Upscale effects from the high-resolution regions on a large-scale circulation outside the refined domain are observed, but the effects are mainly limited to northeastern Asia during the warm season. Together, the results support the multiresolution approach as a computationally efficient and physically consistent method for modeling regional climate.
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      Exploring a Multiresolution Approach Using AMIP Simulations

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    contributor authorSakaguchi, Koichi
    contributor authorLeung, L. Ruby
    contributor authorZhao, Chun
    contributor authorYang, Qing
    contributor authorLu, Jian
    contributor authorHagos, Samson
    contributor authorRauscher, Sara A.
    contributor authorDong, Li
    contributor authorRingler, Todd D.
    contributor authorLauritzen, Peter H.
    date accessioned2017-06-09T17:11:35Z
    date available2017-06-09T17:11:35Z
    date copyright2015/07/01
    date issued2015
    identifier issn0894-8755
    identifier otherams-80873.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4223813
    description abstracthis study presents a diagnosis of a multiresolution approach using the Model for Prediction Across Scales?Atmosphere (MPAS-A) for simulating regional climate. Four Atmospheric Model Intercomparison Project (AMIP) experiments were conducted for 1999?2009. In the first two experiments, MPAS-A was configured using global quasi-uniform grids at 120- and 30-km grid spacing. In the other two experiments, MPAS-A was configured using variable-resolution (VR) mesh with local refinement at 30 km over North America and South America and embedded in a quasi-uniform domain at 120 km elsewhere. Precipitation and related fields in the four simulations are examined to determine how well the VRs reproduce the features simulated by the globally high-resolution model in the refined domain. In previous analyses of idealized aquaplanet simulations, characteristics of the global high-resolution simulation in moist processes developed only near the boundary of the refined region. In contrast, AMIP simulations with VR grids can reproduce high-resolution characteristics across the refined domain, particularly in South America. This finding indicates the importance of finely resolved lower boundary forcings such as topography and surface heterogeneity for regional climate and demonstrates the ability of the MPAS-A VR to replicate the large-scale moisture transport as simulated in the quasi-uniform high-resolution model. Upscale effects from the high-resolution regions on a large-scale circulation outside the refined domain are observed, but the effects are mainly limited to northeastern Asia during the warm season. Together, the results support the multiresolution approach as a computationally efficient and physically consistent method for modeling regional climate.
    publisherAmerican Meteorological Society
    titleExploring a Multiresolution Approach Using AMIP Simulations
    typeJournal Paper
    journal volume28
    journal issue14
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-14-00729.1
    journal fristpage5549
    journal lastpage5574
    treeJournal of Climate:;2015:;volume( 028 ):;issue: 014
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian