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    North American Climate in CMIP5 Experiments. Part I: Evaluation of Historical Simulations of Continental and Regional Climatology

    Source: Journal of Climate:;2013:;volume( 026 ):;issue: 023::page 9209
    Author:
    Sheffield, Justin
    ,
    Barrett, Andrew P.
    ,
    Colle, Brian
    ,
    Nelun Fernando, D.
    ,
    Fu, Rong
    ,
    Geil, Kerrie L.
    ,
    Hu, Qi
    ,
    Kinter, Jim
    ,
    Kumar, Sanjiv
    ,
    Langenbrunner, Baird
    ,
    Lombardo, Kelly
    ,
    Long, Lindsey N.
    ,
    Maloney, Eric
    ,
    Mariotti, Annarita
    ,
    Meyerson, Joyce E.
    ,
    Mo, Kingtse C.
    ,
    David Neelin, J.
    ,
    Nigam, Sumant
    ,
    Pan, Zaitao
    ,
    Ren, Tong
    ,
    Ruiz-Barradas, Alfredo
    ,
    Serra, Yolande L.
    ,
    Seth, Anji
    ,
    Thibeault, Jeanne M.
    ,
    Stroeve, Julienne C.
    ,
    Yang, Ze
    ,
    Yin, Lei
    DOI: 10.1175/JCLI-D-12-00592.1
    Publisher: American Meteorological Society
    Abstract: his is the first part of a three-part paper on North American climate in phase 5 of the Coupled Model Intercomparison Project (CMIP5) that evaluates the historical simulations of continental and regional climatology with a focus on a core set of 17 models. The authors evaluate the models for a set of basic surface climate and hydrological variables and their extremes for the continent. This is supplemented by evaluations for selected regional climate processes relevant to North American climate, including cool season western Atlantic cyclones, the North American monsoon, the U.S. Great Plains low-level jet, and Arctic sea ice. In general, the multimodel ensemble mean represents the observed spatial patterns of basic climate and hydrological variables but with large variability across models and regions in the magnitude and sign of errors. No single model stands out as being particularly better or worse across all analyses, although some models consistently outperform the others for certain variables across most regions and seasons and higher-resolution models tend to perform better for regional processes. The CMIP5 multimodel ensemble shows a slight improvement relative to CMIP3 models in representing basic climate variables, in terms of the mean and spread, although performance has decreased for some models. Improvements in CMIP5 model performance are noticeable for some regional climate processes analyzed, such as the timing of the North American monsoon. The results of this paper have implications for the robustness of future projections of climate and its associated impacts, which are examined in the third part of the paper.
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      North American Climate in CMIP5 Experiments. Part I: Evaluation of Historical Simulations of Continental and Regional Climatology

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4222561
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    contributor authorSheffield, Justin
    contributor authorBarrett, Andrew P.
    contributor authorColle, Brian
    contributor authorNelun Fernando, D.
    contributor authorFu, Rong
    contributor authorGeil, Kerrie L.
    contributor authorHu, Qi
    contributor authorKinter, Jim
    contributor authorKumar, Sanjiv
    contributor authorLangenbrunner, Baird
    contributor authorLombardo, Kelly
    contributor authorLong, Lindsey N.
    contributor authorMaloney, Eric
    contributor authorMariotti, Annarita
    contributor authorMeyerson, Joyce E.
    contributor authorMo, Kingtse C.
    contributor authorDavid Neelin, J.
    contributor authorNigam, Sumant
    contributor authorPan, Zaitao
    contributor authorRen, Tong
    contributor authorRuiz-Barradas, Alfredo
    contributor authorSerra, Yolande L.
    contributor authorSeth, Anji
    contributor authorThibeault, Jeanne M.
    contributor authorStroeve, Julienne C.
    contributor authorYang, Ze
    contributor authorYin, Lei
    date accessioned2017-06-09T17:07:28Z
    date available2017-06-09T17:07:28Z
    date copyright2013/12/01
    date issued2013
    identifier issn0894-8755
    identifier otherams-79747.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4222561
    description abstracthis is the first part of a three-part paper on North American climate in phase 5 of the Coupled Model Intercomparison Project (CMIP5) that evaluates the historical simulations of continental and regional climatology with a focus on a core set of 17 models. The authors evaluate the models for a set of basic surface climate and hydrological variables and their extremes for the continent. This is supplemented by evaluations for selected regional climate processes relevant to North American climate, including cool season western Atlantic cyclones, the North American monsoon, the U.S. Great Plains low-level jet, and Arctic sea ice. In general, the multimodel ensemble mean represents the observed spatial patterns of basic climate and hydrological variables but with large variability across models and regions in the magnitude and sign of errors. No single model stands out as being particularly better or worse across all analyses, although some models consistently outperform the others for certain variables across most regions and seasons and higher-resolution models tend to perform better for regional processes. The CMIP5 multimodel ensemble shows a slight improvement relative to CMIP3 models in representing basic climate variables, in terms of the mean and spread, although performance has decreased for some models. Improvements in CMIP5 model performance are noticeable for some regional climate processes analyzed, such as the timing of the North American monsoon. The results of this paper have implications for the robustness of future projections of climate and its associated impacts, which are examined in the third part of the paper.
    publisherAmerican Meteorological Society
    titleNorth American Climate in CMIP5 Experiments. Part I: Evaluation of Historical Simulations of Continental and Regional Climatology
    typeJournal Paper
    journal volume26
    journal issue23
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-12-00592.1
    journal fristpage9209
    journal lastpage9245
    treeJournal of Climate:;2013:;volume( 026 ):;issue: 023
    contenttypeFulltext
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