Dear regcnet users,
I have run ReGCM-4.1 for six month (March-June)on a domain Meddle East, with EIN15 6-hourly reanalyses and OI_WK SST as
boundary conditions. Although the RegCM4 accurately simulated the spatial distribution in precipitation on all of domain but, it is overestimated over more of domain and the region in comparison with observations.
(figure for 6 month (March-june) total rainfall of ReGCM-4.1 and 4 observations And namelist of model configuration are attached).
-Simplified Kuo (Anthes et al. 1987) -Grell (Grell 1993) -Emanuel (1991) |
Cumulus parameterization scheme |
MEADLE EAST framework -20.0, km horizontal resolution -Central Lat. and Lon. 35.00 °N, 45.00°E –160 (Lat.) ´192 (Lon.) |
Domain
|
Holtslag |
Planetary boundary layer scheme |
||
BATS (Dickinson et al. 1993) |
Land surface model |
Lambert conformal |
Map projection |
23 sigma |
Vertical layers |
2004020100 -2004063000 (6month) |
Simulation period |
SUBEX (Pal et al. 2000) |
Resolved scale precipitation |
'OI_WK', |
Sea Surface Temperature |
Modified CCM3 (Kiehl et al. 1996) |
Radiative transfer |
ERA-Interim (EIN15) |
Boundary data |
Can anybody suggest of tuning any other parameter/variable by which the excessive precipitation over domain may be reduced?
With my best regards,
Kamel azarm