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    The National Hurricane Center Tropical Cyclone Model Guidance Suite

    Source: Weather and Forecasting:;2022:;volume( 037 ):;issue: 011::page 2141
    Author:
    Mark DeMaria
    ,
    James L. Franklin
    ,
    Rachel Zelinsky
    ,
    David A. Zelinsky
    ,
    Matthew J. Onderlinde
    ,
    John A. Knaff
    ,
    Stephanie N. Stevenson
    ,
    John Kaplan
    ,
    Kate D. Musgrave
    ,
    Galina Chirokova
    ,
    Charles R. Sampson
    DOI: 10.1175/WAF-D-22-0039.1
    Publisher: American Meteorological Society
    Abstract: The National Hurricane Center (NHC) uses a variety of guidance models for its operational tropical cyclone track, intensity, and wind structure forecasts, and as baselines for the evaluation of forecast skill. A set of the simpler models, collectively known as the NHC guidance suite, is maintained by NHC. The models comprising the guidance suite are briefly described and evaluated, with details provided for those that have not been documented previously. Decay-SHIFOR is a modified version of the Statistical Hurricane Intensity Forecast (SHIFOR) model that includes decay over land; this modification improves the SHIFOR forecasts through about 96 h. T-CLIPER, a climatology and persistence model that predicts track and intensity using a trajectory approach, has error characteristics similar to those of CLIPER and D-SHIFOR but can be run to any forecast length. The Trajectory and Beta model (TAB), another trajectory track model, applies a gridpoint spatial filter to smooth winds from the National Centers for Environmental Prediction (NCEP) Global Forecast System (GFS) model. TAB model errors were 10%–15% lower than those of the Beta and Advection model (BAM), the model it replaced in 2017. Optimizing TAB’s vertical weights shows that the lower troposphere’s environmental flow provides a better match to observed tropical cyclone motion than does the upper troposphere’s, and that the optimal steering layer is shallower for higher-latitude and weaker tropical cyclones. The advantages and disadvantages of the D-SHIFOR, T-CLIPER, and TAB models relative to their earlier counterparts are discussed.
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      The National Hurricane Center Tropical Cyclone Model Guidance Suite

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    contributor authorMark DeMaria
    contributor authorJames L. Franklin
    contributor authorRachel Zelinsky
    contributor authorDavid A. Zelinsky
    contributor authorMatthew J. Onderlinde
    contributor authorJohn A. Knaff
    contributor authorStephanie N. Stevenson
    contributor authorJohn Kaplan
    contributor authorKate D. Musgrave
    contributor authorGalina Chirokova
    contributor authorCharles R. Sampson
    date accessioned2023-04-12T18:30:17Z
    date available2023-04-12T18:30:17Z
    date copyright2022/11/18
    date issued2022
    identifier otherWAF-D-22-0039.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4289784
    description abstractThe National Hurricane Center (NHC) uses a variety of guidance models for its operational tropical cyclone track, intensity, and wind structure forecasts, and as baselines for the evaluation of forecast skill. A set of the simpler models, collectively known as the NHC guidance suite, is maintained by NHC. The models comprising the guidance suite are briefly described and evaluated, with details provided for those that have not been documented previously. Decay-SHIFOR is a modified version of the Statistical Hurricane Intensity Forecast (SHIFOR) model that includes decay over land; this modification improves the SHIFOR forecasts through about 96 h. T-CLIPER, a climatology and persistence model that predicts track and intensity using a trajectory approach, has error characteristics similar to those of CLIPER and D-SHIFOR but can be run to any forecast length. The Trajectory and Beta model (TAB), another trajectory track model, applies a gridpoint spatial filter to smooth winds from the National Centers for Environmental Prediction (NCEP) Global Forecast System (GFS) model. TAB model errors were 10%–15% lower than those of the Beta and Advection model (BAM), the model it replaced in 2017. Optimizing TAB’s vertical weights shows that the lower troposphere’s environmental flow provides a better match to observed tropical cyclone motion than does the upper troposphere’s, and that the optimal steering layer is shallower for higher-latitude and weaker tropical cyclones. The advantages and disadvantages of the D-SHIFOR, T-CLIPER, and TAB models relative to their earlier counterparts are discussed.
    publisherAmerican Meteorological Society
    titleThe National Hurricane Center Tropical Cyclone Model Guidance Suite
    typeJournal Paper
    journal volume37
    journal issue11
    journal titleWeather and Forecasting
    identifier doi10.1175/WAF-D-22-0039.1
    journal fristpage2141
    journal lastpage2159
    page2141–2159
    treeWeather and Forecasting:;2022:;volume( 037 ):;issue: 011
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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