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    Evaluation of Spatial Errors of Precipitation Rates and Types from TRMM Spaceborne Radar over the Southern CONUS

    Source: Journal of Hydrometeorology:;2013:;Volume( 014 ):;issue: 006::page 1884
    Author:
    Chen, S.
    ,
    Kirstetter, P. E.
    ,
    Hong, Y.
    ,
    Gourley, J. J.
    ,
    Tian, Y. D.
    ,
    Qi, Y. C.
    ,
    Cao, Q.
    ,
    Zhang, J.
    ,
    Howard, K.
    ,
    Hu, J. J.
    ,
    Xue, X. W.
    DOI: 10.1175/JHM-D-13-027.1
    Publisher: American Meteorological Society
    Abstract: n this paper, the authors estimate the uncertainty of the rainfall products from NASA and Japan Aerospace Exploration Agency's (JAXA) Tropical Rainfall Measurement Mission (TRMM) Precipitation Radar (PR) so that they may be used in a quantitative manner for applications like hydrologic modeling or merging with other rainfall products. The spatial error structure of TRMM PR surface rain rates and types was systematically studied by comparing them with NOAA/National Severe Storms Laboratory's (NSSL) next generation, high-resolution (1 km/5 min) National Mosaic and Multi-Sensor Quantitative Precipitation Estimation (QPE; NMQ/Q2) over the TRMM-covered continental United States (CONUS). Data pairs are first matched at the PR footprint scale (5 km/instantaneous) and then grouped into 0.25° grid cells to yield spatially distributed error maps and statistics using data from December 2009 through November 2010. Careful quality control steps (including bias correction with rain gauges and quality filtering) are applied to the ground radar measurements prior to considering them as reference data. The results show that PR captures well the spatial pattern of total rainfall amounts with a high correlation coefficient (CC; 0.91) with Q2, but this decreases to 0.56 for instantaneous rain rates. In terms of precipitation types, Q2 and PR convective echoes are spatially correlated with a CC of 0.63. Despite this correlation, PR's total annual precipitation from convection is 48.82% less than that by Q2, which points to potential issues in the PR algorithm's attenuation correction, nonuniform beam filling, and/or reflectivity-to-rainfall relation. Finally, the spatial analysis identifies regime-dependent errors, in particular in the mountainous west. It is likely that the surface reference technique is triggered over complex terrain, resulting in high-amplitude biases.
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      Evaluation of Spatial Errors of Precipitation Rates and Types from TRMM Spaceborne Radar over the Southern CONUS

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4225054
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    • Journal of Hydrometeorology

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    contributor authorChen, S.
    contributor authorKirstetter, P. E.
    contributor authorHong, Y.
    contributor authorGourley, J. J.
    contributor authorTian, Y. D.
    contributor authorQi, Y. C.
    contributor authorCao, Q.
    contributor authorZhang, J.
    contributor authorHoward, K.
    contributor authorHu, J. J.
    contributor authorXue, X. W.
    date accessioned2017-06-09T17:15:35Z
    date available2017-06-09T17:15:35Z
    date copyright2013/12/01
    date issued2013
    identifier issn1525-755X
    identifier otherams-81991.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4225054
    description abstractn this paper, the authors estimate the uncertainty of the rainfall products from NASA and Japan Aerospace Exploration Agency's (JAXA) Tropical Rainfall Measurement Mission (TRMM) Precipitation Radar (PR) so that they may be used in a quantitative manner for applications like hydrologic modeling or merging with other rainfall products. The spatial error structure of TRMM PR surface rain rates and types was systematically studied by comparing them with NOAA/National Severe Storms Laboratory's (NSSL) next generation, high-resolution (1 km/5 min) National Mosaic and Multi-Sensor Quantitative Precipitation Estimation (QPE; NMQ/Q2) over the TRMM-covered continental United States (CONUS). Data pairs are first matched at the PR footprint scale (5 km/instantaneous) and then grouped into 0.25° grid cells to yield spatially distributed error maps and statistics using data from December 2009 through November 2010. Careful quality control steps (including bias correction with rain gauges and quality filtering) are applied to the ground radar measurements prior to considering them as reference data. The results show that PR captures well the spatial pattern of total rainfall amounts with a high correlation coefficient (CC; 0.91) with Q2, but this decreases to 0.56 for instantaneous rain rates. In terms of precipitation types, Q2 and PR convective echoes are spatially correlated with a CC of 0.63. Despite this correlation, PR's total annual precipitation from convection is 48.82% less than that by Q2, which points to potential issues in the PR algorithm's attenuation correction, nonuniform beam filling, and/or reflectivity-to-rainfall relation. Finally, the spatial analysis identifies regime-dependent errors, in particular in the mountainous west. It is likely that the surface reference technique is triggered over complex terrain, resulting in high-amplitude biases.
    publisherAmerican Meteorological Society
    titleEvaluation of Spatial Errors of Precipitation Rates and Types from TRMM Spaceborne Radar over the Southern CONUS
    typeJournal Paper
    journal volume14
    journal issue6
    journal titleJournal of Hydrometeorology
    identifier doi10.1175/JHM-D-13-027.1
    journal fristpage1884
    journal lastpage1896
    treeJournal of Hydrometeorology:;2013:;Volume( 014 ):;issue: 006
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
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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