Describing the Shape of Raindrop Size Distributions Using Uncorrelated Raindrop Mass Spectrum Parameters

Rainfall retrieval algorithms often assume a gamma-shaped raindrop size distribution (DSD) with three mathematical parametersNw ,Dm , andμ. If only two independent measurements are available, as with the dual-frequency precipitation radar on the Global Precipitation Measurement (GPM) mission core sa...

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Veröffentlicht in:Journal of applied meteorology and climatology 2014-05, Vol.53 (5), p.1282-1296
Hauptverfasser: Williams, Christopher R., Bringi, V. N., Carey, Lawrence D., Chandrasekar, V., Gatlin, Patrick N., Haddad, Ziad S., Meneghini, Robert, Munchak, S. Joseph, Nesbitt, Stephen W., Petersen, Walter A., Tanelli, Simone, Tokay, Ali, Wilson, Anna, Wolff, David B.
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container_end_page 1296
container_issue 5
container_start_page 1282
container_title Journal of applied meteorology and climatology
container_volume 53
creator Williams, Christopher R.
Bringi, V. N.
Carey, Lawrence D.
Chandrasekar, V.
Gatlin, Patrick N.
Haddad, Ziad S.
Meneghini, Robert
Munchak, S. Joseph
Nesbitt, Stephen W.
Petersen, Walter A.
Tanelli, Simone
Tokay, Ali
Wilson, Anna
Wolff, David B.
description Rainfall retrieval algorithms often assume a gamma-shaped raindrop size distribution (DSD) with three mathematical parametersNw ,Dm , andμ. If only two independent measurements are available, as with the dual-frequency precipitation radar on the Global Precipitation Measurement (GPM) mission core satellite, then retrieval algorithms are underconstrained and require assumptions about DSD parameters. To reduce the number of free parameters, algorithms can assume thatμis either a constant or a function ofDm . Previous studies have suggestedμ–Λ constraints [where Λ 5 (4 +μ)/DDm ], but controversies exist over whetherμ–Λ constraints result from physical processes or mathematical artifacts due to high correlations between gamma DSD parameters. This study avoids mathematical artifacts by developing joint probability distribution functions (joint PDFs) of statistically independent DSD attributes derived from the raindrop mass spectrum. These joint PDFs are then mapped into gamma-shaped DSD parameter joint PDFs that can be used in probabilistic rainfall retrieval algorithms as proposed for the GPM satellite program. Surface disdrometer data show a high correlation coefficient between the mass spectrum mean diameterDm and mass spectrum standard deviationσm . To remove correlations between DSD attributes, a normalized mass spectrum standard deviation σ m ' is constructed to be statistically independent ofDm , with σ m ' ¯ representing the most likely value and std ( σ m ' ) representing its dispersion. Joint PDFs ofDm andμare created fromDm and σ m ' . A simple algorithm shows that rain-rate estimates had smaller biases when assuming the DSD breadth of σ m ' ¯ than when assuming a constantμ.
doi_str_mv 10.1175/jamc-d-13-076.1
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To reduce the number of free parameters, algorithms can assume thatμis either a constant or a function ofDm . Previous studies have suggestedμ–Λ constraints [where Λ 5 (4 +μ)/DDm ], but controversies exist over whetherμ–Λ constraints result from physical processes or mathematical artifacts due to high correlations between gamma DSD parameters. This study avoids mathematical artifacts by developing joint probability distribution functions (joint PDFs) of statistically independent DSD attributes derived from the raindrop mass spectrum. These joint PDFs are then mapped into gamma-shaped DSD parameter joint PDFs that can be used in probabilistic rainfall retrieval algorithms as proposed for the GPM satellite program. Surface disdrometer data show a high correlation coefficient between the mass spectrum mean diameterDm and mass spectrum standard deviationσm . To remove correlations between DSD attributes, a normalized mass spectrum standard deviation σ m ' is constructed to be statistically independent ofDm , with σ m ' ¯ representing the most likely value and std ( σ m ' ) representing its dispersion. Joint PDFs ofDm andμare created fromDm and σ m ' . 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N.</au><au>Carey, Lawrence D.</au><au>Chandrasekar, V.</au><au>Gatlin, Patrick N.</au><au>Haddad, Ziad S.</au><au>Meneghini, Robert</au><au>Munchak, S. Joseph</au><au>Nesbitt, Stephen W.</au><au>Petersen, Walter A.</au><au>Tanelli, Simone</au><au>Tokay, Ali</au><au>Wilson, Anna</au><au>Wolff, David B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Describing the Shape of Raindrop Size Distributions Using Uncorrelated Raindrop Mass Spectrum Parameters</atitle><jtitle>Journal of applied meteorology and climatology</jtitle><date>2014-05-01</date><risdate>2014</risdate><volume>53</volume><issue>5</issue><spage>1282</spage><epage>1296</epage><pages>1282-1296</pages><issn>1558-8424</issn><eissn>1558-8432</eissn><coden>JOAMEZ</coden><abstract>Rainfall retrieval algorithms often assume a gamma-shaped raindrop size distribution (DSD) with three mathematical parametersNw ,Dm , andμ. If only two independent measurements are available, as with the dual-frequency precipitation radar on the Global Precipitation Measurement (GPM) mission core satellite, then retrieval algorithms are underconstrained and require assumptions about DSD parameters. To reduce the number of free parameters, algorithms can assume thatμis either a constant or a function ofDm . Previous studies have suggestedμ–Λ constraints [where Λ 5 (4 +μ)/DDm ], but controversies exist over whetherμ–Λ constraints result from physical processes or mathematical artifacts due to high correlations between gamma DSD parameters. This study avoids mathematical artifacts by developing joint probability distribution functions (joint PDFs) of statistically independent DSD attributes derived from the raindrop mass spectrum. These joint PDFs are then mapped into gamma-shaped DSD parameter joint PDFs that can be used in probabilistic rainfall retrieval algorithms as proposed for the GPM satellite program. Surface disdrometer data show a high correlation coefficient between the mass spectrum mean diameterDm and mass spectrum standard deviationσm . To remove correlations between DSD attributes, a normalized mass spectrum standard deviation σ m ' is constructed to be statistically independent ofDm , with σ m ' ¯ representing the most likely value and std ( σ m ' ) representing its dispersion. Joint PDFs ofDm andμare created fromDm and σ m ' . A simple algorithm shows that rain-rate estimates had smaller biases when assuming the DSD breadth of σ m ' ¯ than when assuming a constantμ.</abstract><cop>Boston</cop><pub>American Meteorological Society</pub><doi>10.1175/jamc-d-13-076.1</doi><tpages>15</tpages><oa>free_for_read</oa></addata></record>
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source Jstor Complete Legacy; American Meteorological Society; Alma/SFX Local Collection; EZB Electronic Journals Library
subjects Algorithms
Correlation coefficient
Expected values
Gamma function
Mass spectra
Mathematical analysis
Mathematical independent variables
Meteorology
Precipitation
Probability density functions
Probability distribution
Radar
Radar echoes
Rain
Raindrops
Rainfall
Reflectance
Retrieval
Standard deviation
Studies
title Describing the Shape of Raindrop Size Distributions Using Uncorrelated Raindrop Mass Spectrum Parameters
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