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    Detecting Severe Weather Trends Using an Additive Regressive Convective Hazard Model (AR-CHaMo)

    Source: Journal of Applied Meteorology and Climatology:;2017:;volume 057:;issue 003::page 569
    Author:
    Rädler, Anja T.
    ,
    Groenemeijer, Pieter
    ,
    Faust, Eberhard
    ,
    Sausen, Robert
    DOI: 10.1175/JAMC-D-17-0132.1
    Publisher: American Meteorological Society
    Abstract: AbstractA statistical model for the occurrence of convective hazards was developed and applied to reanalysis data to detect multidecadal trends in hazard frequency. The modeling framework is based on an additive logistic regression for observed hazards that exploits predictors derived from numerical model data. The regression predicts the probability of a severe hazard, which is considered as a product of two components: the probability that a storm occurs and the probability of the severe hazard, given the presence of a storm [P(severe) = P(storm) ? P(severe|storm)]. The model was developed using lightning data as an indication of thunderstorm occurrence and hazard reports across central Europe. Although it uses only two predictors per component, it is capable of reproducing the observed spatial distribution of lightning and yields realistic annual cycles of lightning, hail, and wind fairly accurately. The model was applied to ERA-Interim (1979?2016) across Europe to detect any changes in lightning, hail, and wind hazard occurrence. The frequency of conditions favoring lightning, wind, and large hail has increased across large parts of Europe, with the exception of the southwest. The resulting predicted occurrence of 6-hourly periods with lightning, wind, and large hail has increased by 16%, 29%, and 41%, respectively, across western and central Europe and by 23%, 56%, and 86% across Germany and the Alps during the period considered. It is shown that these changes are caused by increased instability in the reanalysis rather than by changes in midtropospheric moisture or wind shear.
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      Detecting Severe Weather Trends Using an Additive Regressive Convective Hazard Model (AR-CHaMo)

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4261587
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    • Journal of Applied Meteorology and Climatology

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    contributor authorRädler, Anja T.
    contributor authorGroenemeijer, Pieter
    contributor authorFaust, Eberhard
    contributor authorSausen, Robert
    date accessioned2019-09-19T10:06:21Z
    date available2019-09-19T10:06:21Z
    date copyright12/19/2017 12:00:00 AM
    date issued2017
    identifier otherjamc-d-17-0132.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4261587
    description abstractAbstractA statistical model for the occurrence of convective hazards was developed and applied to reanalysis data to detect multidecadal trends in hazard frequency. The modeling framework is based on an additive logistic regression for observed hazards that exploits predictors derived from numerical model data. The regression predicts the probability of a severe hazard, which is considered as a product of two components: the probability that a storm occurs and the probability of the severe hazard, given the presence of a storm [P(severe) = P(storm) ? P(severe|storm)]. The model was developed using lightning data as an indication of thunderstorm occurrence and hazard reports across central Europe. Although it uses only two predictors per component, it is capable of reproducing the observed spatial distribution of lightning and yields realistic annual cycles of lightning, hail, and wind fairly accurately. The model was applied to ERA-Interim (1979?2016) across Europe to detect any changes in lightning, hail, and wind hazard occurrence. The frequency of conditions favoring lightning, wind, and large hail has increased across large parts of Europe, with the exception of the southwest. The resulting predicted occurrence of 6-hourly periods with lightning, wind, and large hail has increased by 16%, 29%, and 41%, respectively, across western and central Europe and by 23%, 56%, and 86% across Germany and the Alps during the period considered. It is shown that these changes are caused by increased instability in the reanalysis rather than by changes in midtropospheric moisture or wind shear.
    publisherAmerican Meteorological Society
    titleDetecting Severe Weather Trends Using an Additive Regressive Convective Hazard Model (AR-CHaMo)
    typeJournal Paper
    journal volume57
    journal issue3
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/JAMC-D-17-0132.1
    journal fristpage569
    journal lastpage587
    treeJournal of Applied Meteorology and Climatology:;2017:;volume 057:;issue 003
    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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