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Proceedings - C-SRNWP Project

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Fig.3 Integration domain for LM-<br />

EURO model.<br />

Domain size 641 x 401<br />

Grid spacing<br />

0.0625 (7 km)<br />

Number of layers 40<br />

Time step and scheme 40 s, 2 time-lev split-expl<br />

Forecast range<br />

60 hrs<br />

Initial time of model run 00 UTC<br />

Lateral bound. condit. IFS<br />

L.B.C. update frequency 3 hr<br />

Initial state<br />

ICNMCA 3DVAR (Interp.)<br />

Initialization<br />

Digital Filter<br />

External analysis<br />

T,u,v, PseudoRH, SP<br />

Special features<br />

Filtered topography<br />

Status<br />

Operational<br />

Hardware<br />

IBM P690 (ECMWF)<br />

N° of processors 120<br />

Table 2 Characteristics of LM-EURO model.<br />

In parallel with the operational configuration of the Lokal Modell described above, an<br />

experimental one has been set up over the Italian domain (LM-ITA, Fig.4 and Table 3).<br />

Fig.4 Integration domain for LM-ITA<br />

model<br />

Domain size 542 x 604<br />

Grid spacing<br />

0.025 (2.8 km)<br />

Number of layers 50<br />

Time step and scheme 30 s 3 time-lev split-expl<br />

Forecast range<br />

48 hrs<br />

Initial time of model run 00 UTC<br />

Lateral bound. condit. LM-EURO<br />

L.B.C. update frequency 1 hr<br />

Initial state<br />

LM-EURO<br />

Initialization<br />

Digital Filter<br />

External analysis<br />

None<br />

Special features<br />

Filtered topography<br />

Status<br />

Experimental<br />

Hardware<br />

IBM P690 (ECMWF)<br />

N° of processors 160<br />

Table 3 Characteristics of LM-ITA model.<br />

The LM-ITA implementation differs from the LM-EURO implementation in terms of both<br />

horizontal (2.8 vs 7 Km) and vertical resolution (50 vs 40 layers). Taking into account the<br />

complex orographic structure of Italy (Fig.5), this increase in resolution should be beneficial<br />

towards a more realistic treatment of near surface parameters and accurate forecast of sensible<br />

weather.<br />

111

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