Describing the Shape of Raindrop Size Distributions Using Uncorrelated Raindrop Mass Spectrum ParametersSource: Journal of Applied Meteorology and Climatology:;2014:;volume( 053 ):;issue: 005::page 1282Author:Williams, Christopher R.
,
Bringi, V. N.
,
Carey, Lawrence D.
,
Chandrasekar, V.
,
Gatlin, Patrick N.
,
Haddad, Ziad S.
,
Meneghini, Robert
,
Joseph Munchak, S.
,
Nesbitt, Stephen W.
,
Petersen, Walter A.
,
Tanelli, Simone
,
Tokay, Ali
,
Wilson, Anna
,
Wolff, David B.
DOI: 10.1175/JAMC-D-13-076.1Publisher: American Meteorological Society
Abstract: ainfall retrieval algorithms often assume a gamma-shaped raindrop size distribution (DSD) with three mathematical parameters Nw, Dm, and ?. 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 that ? is either a constant or a function of Dm. Previous studies have suggested ??? constraints [where ? = (4 + ?)/Dm], but controversies exist over whether ??? 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 diameter Dm and mass spectrum standard deviation σm. To remove correlations between DSD attributes, a normalized mass spectrum standard deviation is constructed to be statistically independent of Dm, with representing the most likely value and std representing its dispersion. Joint PDFs of Dm and ? are created from Dm and . A simple algorithm shows that rain-rate estimates had smaller biases when assuming the DSD breadth of than when assuming a constant ?.
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| contributor author | Williams, Christopher R. | |
| contributor author | Bringi, V. N. | |
| contributor author | Carey, Lawrence D. | |
| contributor author | Chandrasekar, V. | |
| contributor author | Gatlin, Patrick N. | |
| contributor author | Haddad, Ziad S. | |
| contributor author | Meneghini, Robert | |
| contributor author | Joseph Munchak, S. | |
| contributor author | Nesbitt, Stephen W. | |
| contributor author | Petersen, Walter A. | |
| contributor author | Tanelli, Simone | |
| contributor author | Tokay, Ali | |
| contributor author | Wilson, Anna | |
| contributor author | Wolff, David B. | |
| date accessioned | 2017-06-09T16:50:10Z | |
| date available | 2017-06-09T16:50:10Z | |
| date copyright | 2014/05/01 | |
| date issued | 2014 | |
| identifier issn | 1558-8424 | |
| identifier other | ams-75007.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4217296 | |
| description abstract | ainfall retrieval algorithms often assume a gamma-shaped raindrop size distribution (DSD) with three mathematical parameters Nw, Dm, and ?. 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 that ? is either a constant or a function of Dm. Previous studies have suggested ??? constraints [where ? = (4 + ?)/Dm], but controversies exist over whether ??? 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 diameter Dm and mass spectrum standard deviation σm. To remove correlations between DSD attributes, a normalized mass spectrum standard deviation is constructed to be statistically independent of Dm, with representing the most likely value and std representing its dispersion. Joint PDFs of Dm and ? are created from Dm and . A simple algorithm shows that rain-rate estimates had smaller biases when assuming the DSD breadth of than when assuming a constant ?. | |
| publisher | American Meteorological Society | |
| title | Describing the Shape of Raindrop Size Distributions Using Uncorrelated Raindrop Mass Spectrum Parameters | |
| type | Journal Paper | |
| journal volume | 53 | |
| journal issue | 5 | |
| journal title | Journal of Applied Meteorology and Climatology | |
| identifier doi | 10.1175/JAMC-D-13-076.1 | |
| journal fristpage | 1282 | |
| journal lastpage | 1296 | |
| tree | Journal of Applied Meteorology and Climatology:;2014:;volume( 053 ):;issue: 005 | |
| contenttype | Fulltext |