Sensitivity of quantitative precipitation forecasts to boundary layer parameterization: a flash flood case study in theWestern Mediterranean (Articolo in rivista)

Type

• Prodotto della ricerca (Classe)
• Articolo in rivista (Classe)

Label

• Sensitivity of quantitative precipitation forecasts to boundary layer parameterization: a flash flood case study in theWestern Mediterranean (Articolo in rivista) (literal)

Anno

• 2005-01-01T00:00:00+01:00 (literal)

Alternative label

• M. Zampieri, P.Malguzzi, A. Buzzi (2005)
  Sensitivity of quantitative precipitation forecasts to boundary layer parameterization: a flash flood case study in theWestern Mediterranean
  in Natural hazards and earth system sciences (Print)
  (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori

• M. Zampieri, P.Malguzzi, A. Buzzi (literal)

Pagina inizio

• 603 (literal)

Pagina fine

• 612,00 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume

• 5,00 (literal)

Rivista

• Natural hazards and earth system sciences (Rivista)

Note

• ISI Web of Science (WOS) (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni

• ISAC-CNR ISAC-CNR ISAC-CNR (literal)

Titolo

• Sensitivity of quantitative precipitation forecasts to boundary layer parameterization: a flash flood case study in theWestern Mediterranean (literal)

Abstract

• The Montserrat-2000 severe flash flood event which occurred over Catalonia on 9 and 10 June 2000 is analyzed. Strong precipitation was generated by a mesoscale convective system associated with the development of a cyclone. The location of heavy precipitation depends on the position of the cyclone, which, in turn, is found to be very sensitive to various model characteristics and initial conditions. Numerical simulations of this case study using the hydrostatic BOLAM and the non-hydrostatic MOLOCH models are performed in order to test the effects of different formulations of the boundary layer parameterization: a modified version of the Louis (order 1) model and a custom version of the E-l (order 1.5) model. Both of them require a diagnostic formulation of the mixing length, but the use of the turbulent kinetic energy equation in the E-l model allows to represent (literal)

Prodotto di

• Institute of atmospheric sciences and climate (ISAC) (Istituto)
• Meteorologia dinamica (TA.P06.017.003) (Modulo)

Autore CNR

• ANDREA BUZZI (Persona)
• PIERO MALGUZZI (Persona)

Incoming links:

Prodotto

• Institute of atmospheric sciences and climate (ISAC) (Istituto)
• Meteorologia dinamica (TA.P06.017.003) (Modulo)

Autore CNR di

• ANDREA BUZZI (Persona)
• PIERO MALGUZZI (Persona)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#rivistaDi

• Natural hazards and earth system sciences (Rivista)