An evaluation of deep soil configurations in the CLM3 for improved representation of permafrost

Under representation of this feature leads to unrealistic simulation of temperature dynamics in the active layer and permafrost. Using the Community Land Model (CLM3) and its modifications we estimate a required thickness of soil layers to calculate temperature dynamics within certain errors.

Our results show that to compute the annual cycle of temperature dynamics for cold permafrost, the soil thickness should be at least 30 meters. Decadal-to-century time scales require significantly deeper soil layers, e. g. hundreds of meters. We also tested a new geometrical configuration of the soil layer geometry which is called slab permafrost.