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Volumetric soil water content at 50 cm depth with soil moisture stress (SMS) parameterization (middle column in the following table) using ELM differs from those simulated by CLM5 (Figure (a) in the third column in the following table) in Kennedy et al. The discrepancy in soil water simulation between ELM and CLM5 will result in model discrepancy when using plant hydraulic stress (PHS) in ELM. However, similar to CLM5 (Figure a,c in the third column), ELM-PHS simulates wetter soil in the dry season (Figure in the first column) compared to ELM-SMS (Figure in the second column).
| Soil Water Content simulated by ELM PHS | Soil Water Content simulated by ELM SMS | Soil Water Content simulated by CLM5 |
|---|---|---|
 |  |  |
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