Numerical scattering simulations for interpreting simultaneous observations of precipitations by a W-band spaceborne and a C-band ground radar (Contributo in atti di convegno)

Type
Label
  • Numerical scattering simulations for interpreting simultaneous observations of precipitations by a W-band spaceborne and a C-band ground radar (Contributo in atti di convegno) (literal)
Anno
  • 2013-01-01T00:00:00+01:00 (literal)
Alternative label
  • Anna Cinzia Marra (1), Gian Paolo Marra (1) and Franco Prodi (2) (2013)
    Numerical scattering simulations for interpreting simultaneous observations of precipitations by a W-band spaceborne and a C-band ground radar
    in 11th International Precipitation Conference 2013, Ede-Wageningen - The Netherlands, 30 June - 3 July 2013
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Anna Cinzia Marra (1), Gian Paolo Marra (1) and Franco Prodi (2) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • (1) Institute of Atmospheric Sciences and Climate (CNR-ISAC), Strada Provinciale Lecce-Monteroni km 1.2, 73100 - Lecce, Italy (2) Institute of Atmospheric Sciences and Climate (CNR-ISAC), Via P. Gobetti 101, 40129 - Bologna, Italy (literal)
Titolo
  • Numerical scattering simulations for interpreting simultaneous observations of precipitations by a W-band spaceborne and a C-band ground radar (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#isbn
  • 978-94-6173-710-6 (literal)
Abstract
  • The spaceborne W-band (94 GHz) Cloud Profiling Radar (CPR) onboard the CloudSat (CS) satellite, which was launched in 2006, is providing valuable information about global cloud properties. This work aims at interpreting collocated time/space observations from CPR on CS and a ground C-band (5.6 GHz) Radar (GR), with the help of numerical simulations of electromagnetic scattering returns from populations of spheres of ice and liquid water. One precipitating cloud system over Apulia region is investigated. CPR-CS and GR images have been geo-referenced, then combined and displayed for analysis. The numerical simulations of the two radar reflectivities are used as a tool in the inversion procedure, aiming at identifying the hydrometeors, in their phase and size distribution, in the cloud volume simultaneously observed by the two radars. The possible vertical profiles of hydrometeors are presented. (literal)
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