Abstract. Forecasting precipitation over the Mediterranean basin
is still a challenge because of the complex orographic region that
amplifies the need for local observation to correctly initialize the
forecast. In this context, data assimilation techniques play a key role
in improving the initial conditions and consequently the timing and position
of the precipitation forecast. For the first time, the ability of a cycling
4D-Var to reproduce a heavy rain event in central Italy, as well as to
provide a comparison with the largely used cycling 3D-Var, is evaluated in
this study. The radar reflectivity measured by the Italian ground radar
network is assimilated in the Weather Research and Forecasting (WRF) model to simulate an event that occurred on 3 May 2018 in central Italy. In order to evaluate the impact of data
assimilation, several simulations are objectively compared by means of a
fraction skill score (FSS), which is calculated for several threshold
values, and a receiver operating characteristic (ROC) curve. The results
suggest that both assimilation methods in the cycling mode improve the 1-, 3- and
6-hourly quantitative precipitation estimation. More specifically, the
cycling 4D-Var with a warm start initialization shows the highest FSS values
in the first hours of the simulation both with light and heavy precipitation.
Finally, the ROC curve confirms the benefit of 4D-Var: the area under the
curve is 0.91 compared to 0.88 for the control experiment without data
assimilation.
Statistics of the Z–R Relationship for Strong Convective Weather over the Yangtze–Huaihe River Basin and Its Application to Radar Reflectivity Data Assimilation for a Heavy Rain Event
