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    Source: Journal of the Atmospheric Sciences:;2017:;Volume( 074 ):;issue: 011::page 3771
    Author:
    Ying, Yue;Zhang, Fuqing
    DOI: 10.1175/JAS-D-17-0157.1
    Publisher: American Meteorological Society
    Abstract: AbstractThrough a series of convection-permitting regional-scale ensembles based on the Weather Research and Forecasting (WRF) Model, this study investigates the predictability of multiscale weather and convectively coupled equatorial waves during the active phase of a Madden?Julian oscillation (MJO) event over the Indian Ocean from 12 October to 12 November 2011. It is found that the practical predictability limit, estimated by the spread of the ensemble perturbed with realistic initial and boundary uncertainties, is as much as 8 days for horizontal winds, temperature, and humidity for scales larger than 2000 km that include equatorial Rossby, Kelvin, inertia?gravity, and mixed Rossby?gravity waves. The practical predictability limit decreases rapidly as scale decreases, resulting in a predictable time scale less than 1 day for scales smaller than 200 km. Through further experiments using minute initial and boundary perturbations an order of magnitude smaller than the current realistic uncertainties, the intrinsic predictability limit for tropical weather at larger scales (>2000 km) is estimated to be achievable beyond 2 weeks, but the limit is likely still less than 3 days for the small scales (<200 km).
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    contributor authorYing, Yue;Zhang, Fuqing
    date accessioned2018-01-03T11:02:50Z
    date available2018-01-03T11:02:50Z
    date copyright9/12/2017 12:00:00 AM
    date issued2017
    identifier otherjas-d-17-0157.1.pdf
    identifier urihttp://138.201.223.254:8080/yetl1/handle/yetl/4246526
    description abstractAbstractThrough a series of convection-permitting regional-scale ensembles based on the Weather Research and Forecasting (WRF) Model, this study investigates the predictability of multiscale weather and convectively coupled equatorial waves during the active phase of a Madden?Julian oscillation (MJO) event over the Indian Ocean from 12 October to 12 November 2011. It is found that the practical predictability limit, estimated by the spread of the ensemble perturbed with realistic initial and boundary uncertainties, is as much as 8 days for horizontal winds, temperature, and humidity for scales larger than 2000 km that include equatorial Rossby, Kelvin, inertia?gravity, and mixed Rossby?gravity waves. The practical predictability limit decreases rapidly as scale decreases, resulting in a predictable time scale less than 1 day for scales smaller than 200 km. Through further experiments using minute initial and boundary perturbations an order of magnitude smaller than the current realistic uncertainties, the intrinsic predictability limit for tropical weather at larger scales (>2000 km) is estimated to be achievable beyond 2 weeks, but the limit is likely still less than 3 days for the small scales (<200 km).
    publisherAmerican Meteorological Society
    typeJournal Paper
    journal volume74
    journal issue11
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/JAS-D-17-0157.1
    journal fristpage3771
    journal lastpage3785
    treeJournal of the Atmospheric Sciences:;2017:;Volume( 074 ):;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