Data di Pubblicazione:
2000
Abstract:
On 18 June 1997 two simultaneous supercells 50 km apart
swept the Po valley W-NW to E-SE. An exceptional hailfall
lasted for more than 3 hours over a strip 200km wide. There
are no records of companion supercells over northern Italy, a
fact that attributes to the present observations a considerable
meteorological interest.
The forcing due to a baroclinic wave disturbance created
the synoptic conditions favourable for storm development.
A closer mesoscale analysis conducted using the Local
Analysis and Prediction System (LAPS) indicates that the
interaction of the storm systems with the low-level frontal
high-humidity band is a key aspect of their evolution.
The operational polarimetric Doppler weather radar of S.
Pietro Capo®ume was used for a volumetric analysis of the
storm system focusing on the microphysical and dynamical
structure, and wind patterns. Re¯ectivity and Doppler wind
®elds document the transition from multicell to supercell
phase for one of the storms. Differential re¯ectivity (ZDR)
®elds are examined. Positive ZDR columns are detected in
connection with the storms strong updraft. Flare echoes hint
to the presence of substantial hailshafts. The spectrum width
®eld is used to investigate internal motions. Limited dual
Doppler analysis is carried out and results are discussed in
terms of storm evolution properties.
Tipologia CRIS:
01.01 Articolo in rivista
Keywords:
radar; supercell; Doppler
Elenco autori:
Levizzani, Vincenzo
Link alla scheda completa:
Pubblicato in: