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    The Influence of Surface and Precipitation Characteristics on TRMM Microwave Imager Rainfall Retrieval Uncertainty

    Source: Journal of Hydrometeorology:;2015:;Volume( 016 ):;issue: 004::page 1596
    Author:
    Carr, N.
    ,
    Kirstetter, P.-E.
    ,
    Hong, Y.
    ,
    Gourley, J. J.
    ,
    Schwaller, M.
    ,
    Petersen, W.
    ,
    Wang, Nai-Yu
    ,
    Ferraro, Ralph R.
    ,
    Xue, Xianwu
    DOI: 10.1175/JHM-D-14-0194.1
    Publisher: American Meteorological Society
    Abstract: haracterization of the error associated with quantitative precipitation estimates (QPEs) from spaceborne passive microwave (PMW) sensors is important for a variety of applications ranging from flood forecasting to climate monitoring. This study evaluates the joint influence of precipitation and surface characteristics on the error structure of NASA?s Tropical Rainfall Measurement Mission (TRMM) Microwave Imager (TMI) surface QPE product (2A12). TMI precipitation products are compared with high-resolution reference precipitation products obtained from the NOAA/NSSL ground radar?based Multi-Radar Multi-Sensor (MRMS) system. Surface characteristics were represented via a surface classification dataset derived from NASA?s Moderate Resolution Imaging Spectroradiometer (MODIS). This study assesses the ability of 2A12 to detect, classify, and quantify precipitation at its native resolution for the 2011 warm season (March?September) over the southern continental United States. Decreased algorithm performance is apparent over dry and sparsely vegetated regions, a probable result of the surface radiation signal mimicking the scattering signature associated with frozen hydrometeors. Algorithm performance is also shown to be positively correlated with precipitation coverage over the sensor footprint. The algorithm also performs better in pure stratiform and convective precipitation events, compared to events containing a mixture of stratiform and convective precipitation within the footprint. This possibly results from the high spatial gradients of precipitation associated with these events and an underrepresentation of such cases in the retrieval database. The methodology and framework developed herein apply more generally to precipitation estimates from other passive microwave sensors on board low-Earth-orbiting satellites and specifically could be used to evaluate PMW sensors associated with the recently launched Global Precipitation Measurement (GPM) mission.
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      The Influence of Surface and Precipitation Characteristics on TRMM Microwave Imager Rainfall Retrieval Uncertainty

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4225268
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    • Journal of Hydrometeorology

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    contributor authorCarr, N.
    contributor authorKirstetter, P.-E.
    contributor authorHong, Y.
    contributor authorGourley, J. J.
    contributor authorSchwaller, M.
    contributor authorPetersen, W.
    contributor authorWang, Nai-Yu
    contributor authorFerraro, Ralph R.
    contributor authorXue, Xianwu
    date accessioned2017-06-09T17:16:16Z
    date available2017-06-09T17:16:16Z
    date copyright2015/08/01
    date issued2015
    identifier issn1525-755X
    identifier otherams-82182.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4225268
    description abstractharacterization of the error associated with quantitative precipitation estimates (QPEs) from spaceborne passive microwave (PMW) sensors is important for a variety of applications ranging from flood forecasting to climate monitoring. This study evaluates the joint influence of precipitation and surface characteristics on the error structure of NASA?s Tropical Rainfall Measurement Mission (TRMM) Microwave Imager (TMI) surface QPE product (2A12). TMI precipitation products are compared with high-resolution reference precipitation products obtained from the NOAA/NSSL ground radar?based Multi-Radar Multi-Sensor (MRMS) system. Surface characteristics were represented via a surface classification dataset derived from NASA?s Moderate Resolution Imaging Spectroradiometer (MODIS). This study assesses the ability of 2A12 to detect, classify, and quantify precipitation at its native resolution for the 2011 warm season (March?September) over the southern continental United States. Decreased algorithm performance is apparent over dry and sparsely vegetated regions, a probable result of the surface radiation signal mimicking the scattering signature associated with frozen hydrometeors. Algorithm performance is also shown to be positively correlated with precipitation coverage over the sensor footprint. The algorithm also performs better in pure stratiform and convective precipitation events, compared to events containing a mixture of stratiform and convective precipitation within the footprint. This possibly results from the high spatial gradients of precipitation associated with these events and an underrepresentation of such cases in the retrieval database. The methodology and framework developed herein apply more generally to precipitation estimates from other passive microwave sensors on board low-Earth-orbiting satellites and specifically could be used to evaluate PMW sensors associated with the recently launched Global Precipitation Measurement (GPM) mission.
    publisherAmerican Meteorological Society
    titleThe Influence of Surface and Precipitation Characteristics on TRMM Microwave Imager Rainfall Retrieval Uncertainty
    typeJournal Paper
    journal volume16
    journal issue4
    journal titleJournal of Hydrometeorology
    identifier doi10.1175/JHM-D-14-0194.1
    journal fristpage1596
    journal lastpage1614
    treeJournal of Hydrometeorology:;2015:;Volume( 016 ):;issue: 004
    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
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