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    Model Consensus

    Source: Weather and Forecasting:;2000:;volume( 015 ):;issue: 005::page 571
    Author:
    Fritsch, J. M.
    ,
    Hilliker, J.
    ,
    Ross, J.
    ,
    Vislocky, R. L.
    DOI: 10.1175/1520-0434(2000)015<0571:MC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Consensus forecasts from the control runs of several operational numerical models are compared to 1) the control-run forecasts of the individual models that compose the consensus and to 2) other consensus forecasts generated by varying the initial conditions of the various individual models. It is found that the multimodel consensus is superior to the individual control runs and to the consensus forecasts constructed from ensembles of runs generated by varying model initial conditions. The source of the forecast improvement by model consensus is not the result of a simple cancellation of errors as a result of an overall positive bias in one model and an overall negative bias in another. Rather the main improvement stems from overlapping differences in the sign of the errors associated with forecasts of individual traveling disturbances. The results suggest that variations in model physics and numerics play a substantial role in generating the full spectrum of possible solutions that can arise in a given numerical forecast.
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      Model Consensus

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4168857
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    contributor authorFritsch, J. M.
    contributor authorHilliker, J.
    contributor authorRoss, J.
    contributor authorVislocky, R. L.
    date accessioned2017-06-09T14:59:17Z
    date available2017-06-09T14:59:17Z
    date copyright2000/10/01
    date issued2000
    identifier issn0882-8156
    identifier otherams-3141.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4168857
    description abstractConsensus forecasts from the control runs of several operational numerical models are compared to 1) the control-run forecasts of the individual models that compose the consensus and to 2) other consensus forecasts generated by varying the initial conditions of the various individual models. It is found that the multimodel consensus is superior to the individual control runs and to the consensus forecasts constructed from ensembles of runs generated by varying model initial conditions. The source of the forecast improvement by model consensus is not the result of a simple cancellation of errors as a result of an overall positive bias in one model and an overall negative bias in another. Rather the main improvement stems from overlapping differences in the sign of the errors associated with forecasts of individual traveling disturbances. The results suggest that variations in model physics and numerics play a substantial role in generating the full spectrum of possible solutions that can arise in a given numerical forecast.
    publisherAmerican Meteorological Society
    titleModel Consensus
    typeJournal Paper
    journal volume15
    journal issue5
    journal titleWeather and Forecasting
    identifier doi10.1175/1520-0434(2000)015<0571:MC>2.0.CO;2
    journal fristpage571
    journal lastpage582
    treeWeather and Forecasting:;2000:;volume( 015 ):;issue: 005
    contenttypeFulltext
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