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    Initial Results of a Mesoscale Short-Range Ensemble Forecasting System over the Pacific Northwest

    Source: Weather and Forecasting:;2002:;volume( 017 ):;issue: 002::page 192
    Author:
    Grimit, Eric P.
    ,
    Mass, Clifford F.
    DOI: 10.1175/1520-0434(2002)017<0192:IROAMS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Motivated by the promising results of global-scale ensemble forecasting, a number of groups have attempted mesoscale, short-range ensemble forecasting (SREF), focusing mainly over the eastern half of the United States. To evaluate the performance of mesoscale SREF over the Pacific Northwest and to test the value of using different initial analyses as a means of ensemble forecast generation, a five-member mesoscale SREF system was constructed in which the Pennsylvania State University?National Center for Atmospheric Research fifth-generation Mesoscale Model (MM5) was run with initializations and forecast boundary conditions from major operational centers. The ensemble system was evaluated over the Pacific Northwest from January to June 2000. The model verification presented in this study considers only near-surface weather variables, especially the observed 10-m wind direction. The ensemble mean forecast displays lower mean absolute wind direction errors than the component ensemble members when averaged over all cases. The frequency with which the ensemble mean forecast verifies best is no better than the frequency of any individual member forecast. The wind direction forecast errors for the 12-km ensemble mean forecasts are comparable to 4-km deterministic forecast errors. Ensemble mean forecasts are observed to retain much of the orographically forced mesoscale structure in the component forecasts while smoothing out phase differences for propagating features. The correlation between forecast spread and forecast error for wind direction is approximately 0.6 for most lead times. Spread?error correlations rise to roughly 0.8 when only cases with high or low spread are considered. Such high correlations suggest that the ensemble system possesses the ability to predict forecast skill for high- and low-spread cases. The tendency toward higher spread?error correlation when cases with medium spread are filtered out is also found for each component member of the ensemble.
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      Initial Results of a Mesoscale Short-Range Ensemble Forecasting System over the Pacific Northwest

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    contributor authorGrimit, Eric P.
    contributor authorMass, Clifford F.
    date accessioned2017-06-09T15:01:08Z
    date available2017-06-09T15:01:08Z
    date copyright2002/04/01
    date issued2002
    identifier issn0882-8156
    identifier otherams-3224.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4169779
    description abstractMotivated by the promising results of global-scale ensemble forecasting, a number of groups have attempted mesoscale, short-range ensemble forecasting (SREF), focusing mainly over the eastern half of the United States. To evaluate the performance of mesoscale SREF over the Pacific Northwest and to test the value of using different initial analyses as a means of ensemble forecast generation, a five-member mesoscale SREF system was constructed in which the Pennsylvania State University?National Center for Atmospheric Research fifth-generation Mesoscale Model (MM5) was run with initializations and forecast boundary conditions from major operational centers. The ensemble system was evaluated over the Pacific Northwest from January to June 2000. The model verification presented in this study considers only near-surface weather variables, especially the observed 10-m wind direction. The ensemble mean forecast displays lower mean absolute wind direction errors than the component ensemble members when averaged over all cases. The frequency with which the ensemble mean forecast verifies best is no better than the frequency of any individual member forecast. The wind direction forecast errors for the 12-km ensemble mean forecasts are comparable to 4-km deterministic forecast errors. Ensemble mean forecasts are observed to retain much of the orographically forced mesoscale structure in the component forecasts while smoothing out phase differences for propagating features. The correlation between forecast spread and forecast error for wind direction is approximately 0.6 for most lead times. Spread?error correlations rise to roughly 0.8 when only cases with high or low spread are considered. Such high correlations suggest that the ensemble system possesses the ability to predict forecast skill for high- and low-spread cases. The tendency toward higher spread?error correlation when cases with medium spread are filtered out is also found for each component member of the ensemble.
    publisherAmerican Meteorological Society
    titleInitial Results of a Mesoscale Short-Range Ensemble Forecasting System over the Pacific Northwest
    typeJournal Paper
    journal volume17
    journal issue2
    journal titleWeather and Forecasting
    identifier doi10.1175/1520-0434(2002)017<0192:IROAMS>2.0.CO;2
    journal fristpage192
    journal lastpage205
    treeWeather and Forecasting:;2002:;volume( 017 ):;issue: 002
    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
    yabeshDSpacePersian