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contributor authorKirstetter, Pierre-Emmanuel
contributor authorAndrieu, Hervé
contributor authorBoudevillain, Brice
contributor authorDelrieu, Guy
date accessioned2017-06-09T16:49:22Z
date available2017-06-09T16:49:22Z
date copyright2013/07/01
date issued2013
identifier issn1558-8424
identifier otherams-74755.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4217015
description abstracthe vertical profile of reflectivity (VPR) must be identified to correct estimations of rainfall rates by radar for the nonuniform beam filling associated with the vertical variation of radar reflectivity. A method for identifying VPRs from volumetric radar data is presented that takes into account the radar sampling. Physically based constraints on the vertical structure of rainfall are introduced with simple VPR models within a rainfall classification procedure defining more homogeneous precipitation patterns. The model parameters are identified in the framework of an extended Kalman filter to ensure their temporal consistency. The method is assessed using the dataset from a volume-scanning strategy for radar quantitative precipitation estimation designed in 2002 for the Bollène radar (France). The physical consistency of the retrieved VPR is evaluated. Positive results are obtained insofar as the physically based identified VPR (i) presents physically consistent shapes and characteristics considering beam effects, (ii) shows improved robustness in the difficult radar measurement context of the Cévennes?Vivarais region, and (iii) provides consistent physical insight into the rain field.
publisherAmerican Meteorological Society
titleA Physically Based Identification of Vertical Profiles of Reflectivity from Volume Scan Radar Data
typeJournal Paper
journal volume52
journal issue7
journal titleJournal of Applied Meteorology and Climatology
identifier doi10.1175/JAMC-D-12-0228.1
journal fristpage1645
journal lastpage1663
treeJournal of Applied Meteorology and Climatology:;2013:;volume( 052 ):;issue: 007
contenttypeFulltext


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