Application of an adiabatic WRF adjoint to the investigation of the May 2004 McMurdo, Antarctica, severe wind event

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 t...

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Published in:Monthly Weather Review
Other Authors: Xiao, Qingnong (author), Skamarock, Bill (contributor), Kuo, Ying-Hwa (author), Rizvi, Syed (contributor), Ma, Zaizhong (author), Nehrkorn, Thomas (contributor), Huang, Wei (author), Modica, George (contributor), Huang, Xiang-Yu (author), Kaminski, Thomas (contributor), Zhang, Xiaoyan (author), Giering, Ralf (contributor), Barker, Dale (author), Powers, Jordan (contributor), Michalakes, John (author), Manning, Kevin (contributor), Dudhia, Jimy (author), Duda, Michael (contributor), Wee, Tae-Kwon (contributor)
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2008
Subjects:
Online Access:http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-001-421
https://doi.org/10.1175/2008MWR2235.1
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description 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. National Science Foundation (NSF): ...
author2 Xiao, Qingnong (author)
Skamarock, Bill (contributor)
Kuo, Ying-Hwa (author)
Rizvi, Syed (contributor)
Ma, Zaizhong (author)
Nehrkorn, Thomas (contributor)
Huang, Wei (author)
Modica, George (contributor)
Huang, Xiang-Yu (author)
Kaminski, Thomas (contributor)
Zhang, Xiaoyan (author)
Giering, Ralf (contributor)
Barker, Dale (author)
Powers, Jordan (contributor)
Michalakes, John (author)
Manning, Kevin (contributor)
Dudhia, Jimy (author)
Duda, Michael (contributor)
Wee, Tae-Kwon (contributor)
format Article in Journal/Newspaper
title Application of an adiabatic WRF adjoint to the investigation of the May 2004 McMurdo, Antarctica, severe wind event
spellingShingle Application of an adiabatic WRF adjoint to the investigation of the May 2004 McMurdo, Antarctica, severe wind event
title_short Application of an adiabatic WRF adjoint to the investigation of the May 2004 McMurdo, Antarctica, severe wind event
title_full Application of an adiabatic WRF adjoint to the investigation of the May 2004 McMurdo, Antarctica, severe wind event
title_fullStr Application of an adiabatic WRF adjoint to the investigation of the May 2004 McMurdo, Antarctica, severe wind event
title_full_unstemmed Application of an adiabatic WRF adjoint to the investigation of the May 2004 McMurdo, Antarctica, severe wind event
title_sort application of an adiabatic wrf adjoint to the investigation of the may 2004 mcmurdo, antarctica, severe wind event
publisher American Meteorological Society
publishDate 2008
url http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-001-421
https://doi.org/10.1175/2008MWR2235.1
geographic Antarctic
Ross Ice Shelf
South Pole
The Antarctic
West Antarctica
geographic_facet Antarctic
Ross Ice Shelf
South Pole
The Antarctic
West Antarctica
genre Antarc*
Antarctic
Antarctica
Ice Shelf
Ross Ice Shelf
South pole
South pole
West Antarctica
genre_facet Antarc*
Antarctic
Antarctica
Ice Shelf
Ross Ice Shelf
South pole
South pole
West Antarctica
op_relation Monthly Weather Review
http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-001-421
doi:10.1175/2008MWR2235.1
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op_rights Copyright 2008 American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be "fair use" under Section 107 or that satisfies the conditions specified in Section 108 of the U.S. Copyright Law (17 USC, as revised by P.L. 94-553) does not require the Society's permission. Republication, systematic reproduction, posting in electronic form on servers, or other uses of this material, except as exempted by the above statements, requires written permission or license from the AMS. Additional details are provided in the AMS Copyright Policies, available from the AMS at 617-227-2425 or amspubs@ametsoc.org. Permission to place a copy of this work on this server has been provided by the AMS. The AMS does not guarantee that the copy provided here is an accurate copy of the published work.
op_doi https://doi.org/10.1175/2008MWR2235.1
container_title Monthly Weather Review
container_volume 136
container_issue 10
container_start_page 3696
op_container_end_page 3713
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spelling ftncar:oai:drupal-site.org:articles_17324 2024-06-23T07:46:59+00:00 Application of an adiabatic WRF adjoint to the investigation of the May 2004 McMurdo, Antarctica, severe wind event Xiao, Qingnong (author) Skamarock, Bill (contributor) Kuo, Ying-Hwa (author) Rizvi, Syed (contributor) Ma, Zaizhong (author) Nehrkorn, Thomas (contributor) Huang, Wei (author) Modica, George (contributor) Huang, Xiang-Yu (author) Kaminski, Thomas (contributor) Zhang, Xiaoyan (author) Giering, Ralf (contributor) Barker, Dale (author) Powers, Jordan (contributor) Michalakes, John (author) Manning, Kevin (contributor) Dudhia, Jimy (author) Duda, Michael (contributor) Wee, Tae-Kwon (contributor) 2008-10-01 application/pdf http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-001-421 https://doi.org/10.1175/2008MWR2235.1 en eng American Meteorological Society Monthly Weather Review http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-001-421 doi:10.1175/2008MWR2235.1 ark:/85065/d7b56m14 Copyright 2008 American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be "fair use" under Section 107 or that satisfies the conditions specified in Section 108 of the U.S. Copyright Law (17 USC, as revised by P.L. 94-553) does not require the Society's permission. Republication, systematic reproduction, posting in electronic form on servers, or other uses of this material, except as exempted by the above statements, requires written permission or license from the AMS. Additional details are provided in the AMS Copyright Policies, available from the AMS at 617-227-2425 or amspubs@ametsoc.org. Permission to place a copy of this work on this server has been provided by the AMS. The AMS does not guarantee that the copy provided here is an accurate copy of the published work. Text article 2008 ftncar https://doi.org/10.1175/2008MWR2235.1 2024-05-27T14:15:41Z 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. National Science Foundation (NSF): ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Shelf Ross Ice Shelf South pole South pole West Antarctica OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Antarctic Ross Ice Shelf South Pole The Antarctic West Antarctica Monthly Weather Review 136 10 3696 3713