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Using nowcasting technique and data assimilation in a meteorological model to improve very short range hydrological forecasts

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Figure

Figure 1. Area of interest. (a) Location of the radar in the Liguria region and its covered area
Figure 3. Volume trend for rainfall field modification (example for10 November 2014 at 12:00 UTC)
Figure 4. Different blending functions analysed: in panelis the complementary function, used to weight the NWP model forecast
Figure 5. The hydrological nowcasting chain in its three configurations: the first one, which is used only the nowcasted rainfall field withoutvolume modification (a), the second one with the nowcasted rainfall field modified with the trend retrieved by the NWP model (b), and thelast one in which the nowcasted rainfall fields with volume modification are combined through blending with the fields forecasted by NWPmodel corrected with DA (c).
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