Research Article

Influences of Two Land-Surface Schemes on RegCM4 Precipitation Simulations over the Tibetan Plateau

Table 2

Model configuration used in this study.

ContentsDescription

Horizontal grid160 × 108 (Δ = 30 km)
Initial and boundary conditionsERA40, Relaxation (exponential)
Vertical layers (top)23 layers (10 hPa)
Cumulus convectionGrell with Fritsch-Chappell
Turbulence Holtslag scheme
Shortwave/longwave radiationNCAR CCM3
Analysis period1992–2001