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    Application of an Adiabatic WRF Adjoint to the Investigation of the May 2004 McMurdo, Antarctica, Severe Wind Event

    Source: Monthly Weather Review:;2008:;volume( 136 ):;issue: 010::page 3696
    Author:
    Xiao, Qingnong
    ,
    Kuo, Ying-Hwa
    ,
    Ma, Zaizhong
    ,
    Huang, Wei
    ,
    Huang, Xiang-Yu
    ,
    Zhang, Xiaoyan
    ,
    Barker, Dale M.
    ,
    Michalakes, John
    ,
    Dudhia, Jimy
    DOI: 10.1175/2008MWR2235.1
    Publisher: American Meteorological Society
    Abstract: The tangent linear and adjoint of an adiabatic version of the Weather Research and Forecasting (WRF) Model with its Advanced Research WRF (ARW) dynamic core have been developed. The source-to-source automatic differentiation tool [i.e., the Transformation of Algorithm (TAF) in FORTRAN] was used in the development. Tangent linear and adjoint checks of the developed adiabatic WRF adjoint modeling system (WAMS) were conducted, and all necessary correctness verification procedures were passed. As the first application, the adiabatic WAMS was used to study the adjoint sensitivity of a severe windstorm in Antarctica. Linearity tests indicated that an adjoint-based sensitivity study with the Antarctic Mesoscale Prediction System (AMPS) 90-km domain configuration for the windstorm is valid up to 24 h. The adjoint-based sensitivity calculation with adiabatic WAMS identified sensitive regions for the improvement of the 24-h forecast of the windstorm. It is indicated that the windstorm forecast largely relies on the model initial conditions in the area from the south part of the Trans-Antarctic Mountains to West Antarctica and between the Ross Ice Shelf and the South Pole. Based on the sensitivity analysis, the southerly or southeasterly wind at lower levels in the sensitivity region should be larger, the cyclone should be stronger, and the atmospheric stratification should be more stable over the north slope of the Trans-Antarctic Mountain to the Ross Ice Shelf, than the AMPS analyses. By constructing pseudo-observations in the sensitivity region using the gradient information of forecast windstorm intensity around McMurdo, the model initial conditions are revised with the WRF three-dimensional variational data assimilation, which leads to significant improvement in the prediction of the windstorm. An adjoint sensitivity study is an efficient way to identify sensitivity regions in order to collect more observations in the region for better forecasts in a specific aspect of interest.
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      Application of an Adiabatic WRF Adjoint to the Investigation of the May 2004 McMurdo, Antarctica, Severe Wind Event

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4209256
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    • Monthly Weather Review

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    contributor authorXiao, Qingnong
    contributor authorKuo, Ying-Hwa
    contributor authorMa, Zaizhong
    contributor authorHuang, Wei
    contributor authorHuang, Xiang-Yu
    contributor authorZhang, Xiaoyan
    contributor authorBarker, Dale M.
    contributor authorMichalakes, John
    contributor authorDudhia, Jimy
    date accessioned2017-06-09T16:25:56Z
    date available2017-06-09T16:25:56Z
    date copyright2008/10/01
    date issued2008
    identifier issn0027-0644
    identifier otherams-67772.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4209256
    description abstractThe tangent linear and adjoint of an adiabatic version of the Weather Research and Forecasting (WRF) Model with its Advanced Research WRF (ARW) dynamic core have been developed. The source-to-source automatic differentiation tool [i.e., the Transformation of Algorithm (TAF) in FORTRAN] was used in the development. Tangent linear and adjoint checks of the developed adiabatic WRF adjoint modeling system (WAMS) were conducted, and all necessary correctness verification procedures were passed. As the first application, the adiabatic WAMS was used to study the adjoint sensitivity of a severe windstorm in Antarctica. Linearity tests indicated that an adjoint-based sensitivity study with the Antarctic Mesoscale Prediction System (AMPS) 90-km domain configuration for the windstorm is valid up to 24 h. The adjoint-based sensitivity calculation with adiabatic WAMS identified sensitive regions for the improvement of the 24-h forecast of the windstorm. It is indicated that the windstorm forecast largely relies on the model initial conditions in the area from the south part of the Trans-Antarctic Mountains to West Antarctica and between the Ross Ice Shelf and the South Pole. Based on the sensitivity analysis, the southerly or southeasterly wind at lower levels in the sensitivity region should be larger, the cyclone should be stronger, and the atmospheric stratification should be more stable over the north slope of the Trans-Antarctic Mountain to the Ross Ice Shelf, than the AMPS analyses. By constructing pseudo-observations in the sensitivity region using the gradient information of forecast windstorm intensity around McMurdo, the model initial conditions are revised with the WRF three-dimensional variational data assimilation, which leads to significant improvement in the prediction of the windstorm. An adjoint sensitivity study is an efficient way to identify sensitivity regions in order to collect more observations in the region for better forecasts in a specific aspect of interest.
    publisherAmerican Meteorological Society
    titleApplication of an Adiabatic WRF Adjoint to the Investigation of the May 2004 McMurdo, Antarctica, Severe Wind Event
    typeJournal Paper
    journal volume136
    journal issue10
    journal titleMonthly Weather Review
    identifier doi10.1175/2008MWR2235.1
    journal fristpage3696
    journal lastpage3713
    treeMonthly Weather Review:;2008:;volume( 136 ):;issue: 010
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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