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    SAL—A Novel Quality Measure for the Verification of Quantitative Precipitation Forecasts

    Source: Monthly Weather Review:;2008:;volume( 136 ):;issue: 011::page 4470
    Author:
    Wernli, Heini
    ,
    Paulat, Marcus
    ,
    Hagen, Martin
    ,
    Frei, Christoph
    DOI: 10.1175/2008MWR2415.1
    Publisher: American Meteorological Society
    Abstract: A novel object-based quality measure, which contains three distinct components that consider aspects of the structure (S), amplitude (A), and location (L) of the precipitation field in a prespecified domain (e.g., a river catchment) is introduced for the verification of quantitative precipitation forecasts (QPF). This quality measure is referred to as SAL. The amplitude component A measures the relative deviation of the domain-averaged QPF from observations. Positive values of A indicate an overestimation of total precipitation; negative values indicate an underestimation. For the components S and L, coherent precipitation objects are separately identified in the forecast and observations; however, no matching is performed of the objects in the two datasets. The location component L combines information about the displacement of the predicted (compared to the observed) precipitation field?s center of mass and about the error in the weighted-average distance of the precipitation objects from the total field?s center of mass. The structure component S is constructed in such a way that positive values occur if precipitation objects are too large and/or too flat, and negative values if the objects are too small and/or too peaked. Perfect QPFs are characterized by zero values for all components of SAL. Examples with both synthetic precipitation fields and real data are shown to illustrate the concept and characteristics of SAL. SAL is applied to 4 yr of daily accumulated QPFs from a global and finer-scale regional model for a German river catchment, and the SAL diagram is introduced as a compact means of visualizing the results. SAL reveals meaningful information about the systematic differences in the performance of the two models. While the median of the S component is close to zero for the regional model, it is strongly positive for the coarser-scale global model. Consideration is given to the strengths and limitations of the novel quality measure and to possible future applications, in particular, for the verification of QPFs from convection-resolving weather prediction models on short time scales.
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      SAL—A Novel Quality Measure for the Verification of Quantitative Precipitation Forecasts

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4209328
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    • Monthly Weather Review

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    contributor authorWernli, Heini
    contributor authorPaulat, Marcus
    contributor authorHagen, Martin
    contributor authorFrei, Christoph
    date accessioned2017-06-09T16:26:08Z
    date available2017-06-09T16:26:08Z
    date copyright2008/11/01
    date issued2008
    identifier issn0027-0644
    identifier otherams-67837.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4209328
    description abstractA novel object-based quality measure, which contains three distinct components that consider aspects of the structure (S), amplitude (A), and location (L) of the precipitation field in a prespecified domain (e.g., a river catchment) is introduced for the verification of quantitative precipitation forecasts (QPF). This quality measure is referred to as SAL. The amplitude component A measures the relative deviation of the domain-averaged QPF from observations. Positive values of A indicate an overestimation of total precipitation; negative values indicate an underestimation. For the components S and L, coherent precipitation objects are separately identified in the forecast and observations; however, no matching is performed of the objects in the two datasets. The location component L combines information about the displacement of the predicted (compared to the observed) precipitation field?s center of mass and about the error in the weighted-average distance of the precipitation objects from the total field?s center of mass. The structure component S is constructed in such a way that positive values occur if precipitation objects are too large and/or too flat, and negative values if the objects are too small and/or too peaked. Perfect QPFs are characterized by zero values for all components of SAL. Examples with both synthetic precipitation fields and real data are shown to illustrate the concept and characteristics of SAL. SAL is applied to 4 yr of daily accumulated QPFs from a global and finer-scale regional model for a German river catchment, and the SAL diagram is introduced as a compact means of visualizing the results. SAL reveals meaningful information about the systematic differences in the performance of the two models. While the median of the S component is close to zero for the regional model, it is strongly positive for the coarser-scale global model. Consideration is given to the strengths and limitations of the novel quality measure and to possible future applications, in particular, for the verification of QPFs from convection-resolving weather prediction models on short time scales.
    publisherAmerican Meteorological Society
    titleSAL—A Novel Quality Measure for the Verification of Quantitative Precipitation Forecasts
    typeJournal Paper
    journal volume136
    journal issue11
    journal titleMonthly Weather Review
    identifier doi10.1175/2008MWR2415.1
    journal fristpage4470
    journal lastpage4487
    treeMonthly Weather Review:;2008:;volume( 136 ):;issue: 011
    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