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    A Dynamic and Spatial Scaling Approach to Advection Forecasting

    Source: Journal of Applied Meteorology:;2003:;volume( 042 ):;issue: 003::page 381
    Author:
    Seed, A. W.
    DOI: 10.1175/1520-0450(2003)042<0381:ADASSA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Quantitative nowcasts of rainfall are frequently based on the advection of rain fields observed by weather radar. Spectral Prognosis (S-PROG) is an advection-based nowcasting system that uses the observations that rain fields commonly exhibit both spatial and dynamic scaling properties, that is, the lifetime of a feature in the field is dependent on the scale of the feature (large features evolve more slowly than small features), and that features at all scales between the outer and inner observed scales are present in the field. The logarithm of the radar reflectivity field is disaggregated into a set or cascade of fields, in which each field in the set (or level in the cascade) represents the features of the original field over a limited range of scales. The Lagrangian temporal evolution of each level in the cascade is modeled using a simple autoregressive (lag 2) model, which automatically causes the forecast field to become smooth as the structures at the various scales evolve through their life cycles, or can be used to generate conditional simulations if the noise term is included. This paper describes the model and presents preliminary results.
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      A Dynamic and Spatial Scaling Approach to Advection Forecasting

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4148658
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    contributor authorSeed, A. W.
    date accessioned2017-06-09T14:08:42Z
    date available2017-06-09T14:08:42Z
    date copyright2003/03/01
    date issued2003
    identifier issn0894-8763
    identifier otherams-13230.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148658
    description abstractQuantitative nowcasts of rainfall are frequently based on the advection of rain fields observed by weather radar. Spectral Prognosis (S-PROG) is an advection-based nowcasting system that uses the observations that rain fields commonly exhibit both spatial and dynamic scaling properties, that is, the lifetime of a feature in the field is dependent on the scale of the feature (large features evolve more slowly than small features), and that features at all scales between the outer and inner observed scales are present in the field. The logarithm of the radar reflectivity field is disaggregated into a set or cascade of fields, in which each field in the set (or level in the cascade) represents the features of the original field over a limited range of scales. The Lagrangian temporal evolution of each level in the cascade is modeled using a simple autoregressive (lag 2) model, which automatically causes the forecast field to become smooth as the structures at the various scales evolve through their life cycles, or can be used to generate conditional simulations if the noise term is included. This paper describes the model and presents preliminary results.
    publisherAmerican Meteorological Society
    titleA Dynamic and Spatial Scaling Approach to Advection Forecasting
    typeJournal Paper
    journal volume42
    journal issue3
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(2003)042<0381:ADASSA>2.0.CO;2
    journal fristpage381
    journal lastpage388
    treeJournal of Applied Meteorology:;2003:;volume( 042 ):;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
    yabeshDSpacePersian