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    Morphology, Intensity, and Rainfall Production of MJO Convection: Observations from DYNAMO Shipborne Radar and TRMM

    Source: Journal of the Atmospheric Sciences:;2014:;Volume( 072 ):;issue: 002::page 623
    Author:
    Xu, Weixin
    ,
    Rutledge, Steven A.
    DOI: 10.1175/JAS-D-14-0130.1
    Publisher: American Meteorological Society
    Abstract: his study uses Dynamics of the Madden?Julian Oscillation (DYNAMO) shipborne [Research Vessel (R/V) Roger Revelle] radar and Tropical Rainfall Measuring Mission (TRMM) Precipitation Radar (PR) datasets to investigate MJO-associated convective systems in specific organizational modes [mesoscale convective system (MCS) versus sub-MCS and linear versus nonlinear]. The Revelle radar sampled many ?climatological? aspects of MJO convection as indicated by comparison with the long-term TRMM PR statistics, including areal-mean rainfall (6?7 mm day?1), convective intensity, rainfall contributions from different morphologies, and their variations with MJO phase. Nonlinear sub-MCSs were present 70% of the time but contributed just around 20% of the total rainfall. In contrast, linear and nonlinear MCSs were present 10% of the time but contributed 20% and 50%, respectively. These distributions vary with MJO phase, with the largest sub-MCS rainfall fraction in suppressed phases (phases 5?7) and maximum MCS precipitation in active phases (phases 2 and 3). Similarly, convective?stratiform rainfall fractions also varied significantly with MJO phase, with the highest convective fractions (70%?80%) in suppressed phases and the largest stratiform fraction (40%?50%) in active phases. However, there are also discrepancies between the Revelle radar and TRMM PR. Revelle radar data indicated a mean convective rain fraction of 70% compared to 55% for TRMM PR. This difference is mainly due to the reduced resolution of the TRMM PR compared to the ship radar. There are also notable differences in the rainfall contributions as a function of convective intensity between the Revelle radar and TRMM PR. In addition, TRMM PR composites indicate linear MCS rainfall increases after MJO onset and produce similar rainfall contributions to nonlinear MCSs; however, the Revelle radar statistics show the clear dominance of nonlinear MCS rainfall.
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      Morphology, Intensity, and Rainfall Production of MJO Convection: Observations from DYNAMO Shipborne Radar and TRMM

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4219612
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    contributor authorXu, Weixin
    contributor authorRutledge, Steven A.
    date accessioned2017-06-09T16:57:40Z
    date available2017-06-09T16:57:40Z
    date copyright2015/02/01
    date issued2014
    identifier issn0022-4928
    identifier otherams-77092.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4219612
    description abstracthis study uses Dynamics of the Madden?Julian Oscillation (DYNAMO) shipborne [Research Vessel (R/V) Roger Revelle] radar and Tropical Rainfall Measuring Mission (TRMM) Precipitation Radar (PR) datasets to investigate MJO-associated convective systems in specific organizational modes [mesoscale convective system (MCS) versus sub-MCS and linear versus nonlinear]. The Revelle radar sampled many ?climatological? aspects of MJO convection as indicated by comparison with the long-term TRMM PR statistics, including areal-mean rainfall (6?7 mm day?1), convective intensity, rainfall contributions from different morphologies, and their variations with MJO phase. Nonlinear sub-MCSs were present 70% of the time but contributed just around 20% of the total rainfall. In contrast, linear and nonlinear MCSs were present 10% of the time but contributed 20% and 50%, respectively. These distributions vary with MJO phase, with the largest sub-MCS rainfall fraction in suppressed phases (phases 5?7) and maximum MCS precipitation in active phases (phases 2 and 3). Similarly, convective?stratiform rainfall fractions also varied significantly with MJO phase, with the highest convective fractions (70%?80%) in suppressed phases and the largest stratiform fraction (40%?50%) in active phases. However, there are also discrepancies between the Revelle radar and TRMM PR. Revelle radar data indicated a mean convective rain fraction of 70% compared to 55% for TRMM PR. This difference is mainly due to the reduced resolution of the TRMM PR compared to the ship radar. There are also notable differences in the rainfall contributions as a function of convective intensity between the Revelle radar and TRMM PR. In addition, TRMM PR composites indicate linear MCS rainfall increases after MJO onset and produce similar rainfall contributions to nonlinear MCSs; however, the Revelle radar statistics show the clear dominance of nonlinear MCS rainfall.
    publisherAmerican Meteorological Society
    titleMorphology, Intensity, and Rainfall Production of MJO Convection: Observations from DYNAMO Shipborne Radar and TRMM
    typeJournal Paper
    journal volume72
    journal issue2
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/JAS-D-14-0130.1
    journal fristpage623
    journal lastpage640
    treeJournal of the Atmospheric Sciences:;2014:;Volume( 072 ):;issue: 002
    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