1. Latest results in the precipitation verification over Northern Italy Elena Oberto, Marco Turco, Paolo Bertolotto (*) ARPA Piemonte, Torino, Italy

2. Objectives Verification over NI: 1.Seasonal daily cycle and seasonal statistical indices over 47 basins: 00/12 UTC run, forecast time: +24, +48, 6h diurnal cycle 2.Seasonal statistical indices over mountain/plain basins 3.Seasonal statistical indices over western/eastern basins LM-DWD, aLMo, LAMI over Northern Italy LAMI vs. LAMI prog prec over Piedmont Comparative precipitation verification LAMI study: 1.LAMI vs. LAMI with prog. Prec verification: performance comparison over Piedmont basins from August 2004 to July 2005 2.Seasonal statistical indices and cumulated precipitation maps 3.Application to a foehn case study.

3. Piedmont: percentage valid data (August 2004-July 2005) Eastern Italian basins Western Italian basins Plain Italian basins Mountain Italian basins

4. Seasonal trend over NI: run00 5 mm

5. 10 mm Seasonal trend over Northern Italy- run00

6. Seasonal trend over NI: run12 5 mm

7. 10 mm

8. Seasonal trend over Northern Italy: different performance over plain and mountainous areas 10 mm

9. Seasonal trend over Northern Italy: different performance over western and eastern areas 10 mm

10. Seasonal daily cycle over NI

11. Remarks General worsening during last seasons, exp. DJF’05: there is an increasing in QPF (due to the introduction of prog. cloud ice scheme?), BUT  DJF ’04 ~ 400 events > 10mm/24h on the average DJF ’05 ~ 150 events > 10mm/24h on the average  110 on the East, 40 on the West 1) How many does an halved statistics affect the results interpretation? 2) How much is more difficult to estimate quantitatively the precipitation during a particularly dry winter with respect to a “normal” winter? The role of soil moisture analisys during summer seasons seems to be decisive in term of QPF (better BIAS index for LM-DWD in JJA) but not in term of capability to localize and predict accurately the precipitation pattern (ETS very low) Big differences in term of BIAS between mountainous and plain areas: we obtain a greater overestimation on the mountain, except for LAMI in DJF’05: only LAMI runs without prog. prec.: to investigate the behaviour of prognostic precipitation during very dry season. Different trend on the West and East areas: 1.aLMo  general increasing in QPF, but much greater overestimation on Western areas 2.LK-DWD  general increasing in QPF during last seasons, slightly greater overestimation on Western areas 3.LAMI  behaviour similar to the other version, but not for DJF’05: big overestimation on the East where we have the greater majority of precipitation cases.

12. LAMI study “PROGNOSTIC PRECIPITATION” version (lam00) vs. STANDARD (nud00) Domain study: Piedmont basins (with Ticino raingauges) Period study: August 2004-July 2005

13. BIAS and ETS: Forecast time D+2 Lam00  prog prec version Nud00  standard version Aug’04/Jul’05 The error bars indicates 2.5th and 97.5th percentiles of resampled distribution, applied to the "reference" model.

14. Aug’04/Jul’05 Lam00  prog prec version Nud00  standard version HRR and FAR: Forecast time D+2

15. SON ‘04 BIAS and ETS: Forecast time D+2 Lam00  prog prec version Nud00  standard version

16. SON ‘04 HRR and FAR: Forecast time D+2 Lam00  prog prec version Nud00  standard version

17. November 2004 observed LAMI prognostic rain scheme LAMI “standard”

18. DJF ‘05 BIAS and ETS: Forecast time D+2 Lam00  prog prec version Nud00  standard version

19. DJF ‘05 HRR and FAR: Forecast time D+2 Lam00  prog prec version Nud00  standard version

20. Case study during a strong foehn event: 21-22 Jan’05 LAMI prognostic rain scheme LAMI “standard” Observed

21. MAM ‘05 BIAS and ETS: Forecast time D+2 Lam00  prog prec version Nud00  standard version

22. Lam00  prog prec version Nud00  standard version HRR and FAR: Forecast time D+2 MAM ‘05

23. Seasonal comparison LAMI vs. LAMI prog Scale (mm)

24. Remarks Aug’04-Jul’05  globally for high thresholds the BIAS is significantly reduced Seasonal trend: the BIAS reduction is noticeable during wet season and for moderate/strong precipitation The prognostic scheme seems to not solve completely the underestimation downwind but it reduces the overestimation upwind DJF ’05  slightly worsening of LAMI prog., particularly over north-western alpine chain, that represents in this case the “downwind side” (north-western flux as prevailing synoptic situation)!