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    A Characterization of the Present-Day Arctic Atmosphere in CCSM4

    Source: Journal of Climate:;2011:;volume( 025 ):;issue: 008::page 2676
    Author:
    de Boer, Gijs
    ,
    Chapman, William
    ,
    Kay, Jennifer E.
    ,
    Medeiros, Brian
    ,
    Shupe, Matthew D.
    ,
    Vavrus, Steve
    ,
    Walsh, John
    DOI: 10.1175/JCLI-D-11-00228.1
    Publisher: American Meteorological Society
    Abstract: imulation of key features of the Arctic atmosphere in the Community Climate System Model, version 4 (CCSM4) is evaluated against observational and reanalysis datasets for the present-day (1981?2005). Surface air temperature, sea level pressure, cloud cover and phase, precipitation and evaporation, the atmospheric energy budget, and lower-tropospheric stability are evaluated. Simulated surface air temperatures are found to be slightly too cold when compared with the 40-yr ECMWF Re-Analysis (ERA-40). Spatial patterns and temporal variability are well simulated. Evaluation of the sea level pressure demonstrates some large biases, most noticeably an under simulation of the Beaufort High during spring and autumn. Monthly Arctic-wide biases of up to 13 mb are reported. Cloud cover is underpredicted for all but summer months, and cloud phase is demonstrated to be different from observations. Despite low cloud cover, simulated all-sky liquid water paths are too high, while ice water path was generally too low. Precipitation is found to be excessive over much of the Arctic compared to ERA-40 and the Global Precipitation Climatology Project (GPCP) estimates. With some exceptions, evaporation is well captured by CCSM4, resulting in P ? E estimates that are too high. CCSM4 energy budget terms show promising agreement with estimates from several sources. The most noticeable exception to this is the top of the atmosphere (TOA) fluxes that are found to be too low while surface fluxes are found to be too high during summer months. Finally, the lower troposphere is found to be too stable when compared to ERA-40 during all times of year but particularly during spring and summer months.
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      A Characterization of the Present-Day Arctic Atmosphere in CCSM4

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4221694
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    contributor authorde Boer, Gijs
    contributor authorChapman, William
    contributor authorKay, Jennifer E.
    contributor authorMedeiros, Brian
    contributor authorShupe, Matthew D.
    contributor authorVavrus, Steve
    contributor authorWalsh, John
    date accessioned2017-06-09T17:04:23Z
    date available2017-06-09T17:04:23Z
    date copyright2012/04/01
    date issued2011
    identifier issn0894-8755
    identifier otherams-78967.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4221694
    description abstractimulation of key features of the Arctic atmosphere in the Community Climate System Model, version 4 (CCSM4) is evaluated against observational and reanalysis datasets for the present-day (1981?2005). Surface air temperature, sea level pressure, cloud cover and phase, precipitation and evaporation, the atmospheric energy budget, and lower-tropospheric stability are evaluated. Simulated surface air temperatures are found to be slightly too cold when compared with the 40-yr ECMWF Re-Analysis (ERA-40). Spatial patterns and temporal variability are well simulated. Evaluation of the sea level pressure demonstrates some large biases, most noticeably an under simulation of the Beaufort High during spring and autumn. Monthly Arctic-wide biases of up to 13 mb are reported. Cloud cover is underpredicted for all but summer months, and cloud phase is demonstrated to be different from observations. Despite low cloud cover, simulated all-sky liquid water paths are too high, while ice water path was generally too low. Precipitation is found to be excessive over much of the Arctic compared to ERA-40 and the Global Precipitation Climatology Project (GPCP) estimates. With some exceptions, evaporation is well captured by CCSM4, resulting in P ? E estimates that are too high. CCSM4 energy budget terms show promising agreement with estimates from several sources. The most noticeable exception to this is the top of the atmosphere (TOA) fluxes that are found to be too low while surface fluxes are found to be too high during summer months. Finally, the lower troposphere is found to be too stable when compared to ERA-40 during all times of year but particularly during spring and summer months.
    publisherAmerican Meteorological Society
    titleA Characterization of the Present-Day Arctic Atmosphere in CCSM4
    typeJournal Paper
    journal volume25
    journal issue8
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-11-00228.1
    journal fristpage2676
    journal lastpage2695
    treeJournal of Climate:;2011:;volume( 025 ):;issue: 008
    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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