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    Error Structure of Multiparameter Radar and Surface Measurements of Rainfall Part II: X-Band Attenuation

    Source: Journal of Atmospheric and Oceanic Technology:;1988:;volume( 005 ):;issue: 006::page 796
    Author:
    Chandrasekar, V.
    ,
    Bringi, V. N.
    DOI: 10.1175/1520-0426(1988)005<0796:ESOMRA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In Part II of this study, simulations of multiparameter radar observables to include X-band specific attenuation (A) are performed in order to study the relationship between A, Z, and ZDR. We also compute the triplet (A, Z, ZDR) from simulations of disdrometer raindrop spectra. As in Part I, our simulations include the fluctuations due to both measurement errors and physical variations of the gamma raindrop spectra parameters (N0, D0, m). We examine the correlation between (A/Z) and ZDR derived from both disdrometer and radar simulations, and show that the disdrometer-based data yields a negative collation (? ?0.9) between (A/Z) and ZDR, whereas for radar data the correlation ≈ 0. We emphasize that these correlations are due only to measurement fluctuations, and not to physical variations. The large magnitude for the negative correlation compresses the scatter in plots of (A/Z) versus ZDR based on disdrometer RSD samples whereas the same scatter plots using multiparameter radar data show very large scatter. We also simulate A, Z and ZDR from three separate disdrometers (all sampling the same gamma RSD) and show that the scatter is more realistic and much larger than when using a single disdrometer.
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      Error Structure of Multiparameter Radar and Surface Measurements of Rainfall Part II: X-Band Attenuation

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4180623
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    contributor authorChandrasekar, V.
    contributor authorBringi, V. N.
    date accessioned2017-06-09T15:22:36Z
    date available2017-06-09T15:22:36Z
    date copyright1988/12/01
    date issued1988
    identifier issn0739-0572
    identifier otherams-420.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4180623
    description abstractIn Part II of this study, simulations of multiparameter radar observables to include X-band specific attenuation (A) are performed in order to study the relationship between A, Z, and ZDR. We also compute the triplet (A, Z, ZDR) from simulations of disdrometer raindrop spectra. As in Part I, our simulations include the fluctuations due to both measurement errors and physical variations of the gamma raindrop spectra parameters (N0, D0, m). We examine the correlation between (A/Z) and ZDR derived from both disdrometer and radar simulations, and show that the disdrometer-based data yields a negative collation (? ?0.9) between (A/Z) and ZDR, whereas for radar data the correlation ≈ 0. We emphasize that these correlations are due only to measurement fluctuations, and not to physical variations. The large magnitude for the negative correlation compresses the scatter in plots of (A/Z) versus ZDR based on disdrometer RSD samples whereas the same scatter plots using multiparameter radar data show very large scatter. We also simulate A, Z and ZDR from three separate disdrometers (all sampling the same gamma RSD) and show that the scatter is more realistic and much larger than when using a single disdrometer.
    publisherAmerican Meteorological Society
    titleError Structure of Multiparameter Radar and Surface Measurements of Rainfall Part II: X-Band Attenuation
    typeJournal Paper
    journal volume5
    journal issue6
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1988)005<0796:ESOMRA>2.0.CO;2
    journal fristpage796
    journal lastpage802
    treeJournal of Atmospheric and Oceanic Technology:;1988:;volume( 005 ):;issue: 006
    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