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    Energy Transformation and Diabatic Processes in Developing and Nondeveloping African Easterly Waves Observed during the NAMMA Project of 2006

    Source: Weather and Forecasting:;2009:;volume( 024 ):;issue: 006::page 1524
    Author:
    Ross, Robert S.
    ,
    Krishnamurti, T. N.
    ,
    Pattnaik, S.
    ,
    Simon, A.
    DOI: 10.1175/2009WAF2222235.1
    Publisher: American Meteorological Society
    Abstract: This paper provides an understanding of essential differences between developing and nondeveloping African easterly waves, which was a major goal of NAMMA, NASA?s field program in the eastern Atlantic, which functioned as an extension of the African Monsoon Multidisciplinary Analysis (AMMA) program during 2006. Three NAMMA waves are studied in detail using FNL analysis: NAMMA wave 2, which developed into Tropical Storm Debby; NAMMA wave 7, which developed into Hurricane Helene; and NAMMA wave 4, which did not develop within the NAMMA domain. Diagnostic calculations are performed on the analyzed fields using energy transformation equations and the isentropic potential vorticity equation. The results show that the two developing waves possess clear and robust positive barotropic energy conversion in conjunction with positive diabatic heating that includes a singular burst of heating at a particular time in the wave?s history. This positive barotropic energy conversion is facilitated in waves that have a northeast?southwest tilt to the trough axis and a wind maximum to the west of this axis. The nondeveloping wave is found to have the same singular burst of diabatic heating at one point in its history, but development of the wave does not occur due to negative barotropic energy conversion. Such conversion is facilitated by a northwest?southeast tilt to the trough axis and a wind maximum to the east of this axis. The conclusions about wave development and nondevelopment formulated in this research are viewed as important and significant, but they require additional testing with detailed observational- and numerical-based studies.
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      Energy Transformation and Diabatic Processes in Developing and Nondeveloping African Easterly Waves Observed during the NAMMA Project of 2006

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4211434
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    contributor authorRoss, Robert S.
    contributor authorKrishnamurti, T. N.
    contributor authorPattnaik, S.
    contributor authorSimon, A.
    date accessioned2017-06-09T16:32:45Z
    date available2017-06-09T16:32:45Z
    date copyright2009/12/01
    date issued2009
    identifier issn0882-8156
    identifier otherams-69732.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4211434
    description abstractThis paper provides an understanding of essential differences between developing and nondeveloping African easterly waves, which was a major goal of NAMMA, NASA?s field program in the eastern Atlantic, which functioned as an extension of the African Monsoon Multidisciplinary Analysis (AMMA) program during 2006. Three NAMMA waves are studied in detail using FNL analysis: NAMMA wave 2, which developed into Tropical Storm Debby; NAMMA wave 7, which developed into Hurricane Helene; and NAMMA wave 4, which did not develop within the NAMMA domain. Diagnostic calculations are performed on the analyzed fields using energy transformation equations and the isentropic potential vorticity equation. The results show that the two developing waves possess clear and robust positive barotropic energy conversion in conjunction with positive diabatic heating that includes a singular burst of heating at a particular time in the wave?s history. This positive barotropic energy conversion is facilitated in waves that have a northeast?southwest tilt to the trough axis and a wind maximum to the west of this axis. The nondeveloping wave is found to have the same singular burst of diabatic heating at one point in its history, but development of the wave does not occur due to negative barotropic energy conversion. Such conversion is facilitated by a northwest?southeast tilt to the trough axis and a wind maximum to the east of this axis. The conclusions about wave development and nondevelopment formulated in this research are viewed as important and significant, but they require additional testing with detailed observational- and numerical-based studies.
    publisherAmerican Meteorological Society
    titleEnergy Transformation and Diabatic Processes in Developing and Nondeveloping African Easterly Waves Observed during the NAMMA Project of 2006
    typeJournal Paper
    journal volume24
    journal issue6
    journal titleWeather and Forecasting
    identifier doi10.1175/2009WAF2222235.1
    journal fristpage1524
    journal lastpage1548
    treeWeather and Forecasting:;2009:;volume( 024 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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