Precipitation classification at mid-latitudes in terms of drop size distribution parameters (Articolo in rivista)

Type
Label
  • Precipitation classification at mid-latitudes in terms of drop size distribution parameters (Articolo in rivista) (literal)
Anno
  • 2008-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.5194/adgeo-16-11-2008 (literal)
Alternative label
  • Caracciolo C.; F. Porcù; F. Prodi (2008)
    Precipitation classification at mid-latitudes in terms of drop size distribution parameters
    in Advances in geosciences (Print)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Caracciolo C.; F. Porcù; F. Prodi (literal)
Pagina inizio
  • 11 (literal)
Pagina fine
  • 17 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 16 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
  • 7 (literal)
Note
  • Scopus (literal)
  • Google Scholar (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • dipartimento di fisica università di ferrara (literal)
Titolo
  • Precipitation classification at mid-latitudes in terms of drop size distribution parameters (literal)
Abstract
  • The drop size distribution (DSD) is a fundamental property of rainfall because the shape of the distribution reflects the physics of rain formation processes. Given the lack of studies on the DSD at mid-latitudes, the present work focuses on the microphysical characterization of precipitation events occurring in Italy, using two different types of disdrometer. A large number of different rain events was collected: they underwent microphysical analysis by computing the Z-R relationships, observing the average DSDs and DSD parameters, fitting the real distribution for different rainfall rate categories and applying convective (C) - stratiform (S) discrimination algorithms. A general agreement with past works at mid-latitudes is found both in the Z-R relationship and in DSD parameters. The rain distribution is well described by a gamma DSD and only in some cases (especially the light rain events) by an exponential DSD. Marked differences are observed in DSD parameters and Z-R relationships between C and S episodes. The use of disdrometers for areas covered by multiparametric radar is suggested and will be performed in the near future (literal)
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