实现了陆面过程模型 SiB2 和 AquiferFlow 的耦合，显著增强了对地表-地下水相互作用和蒸散发的模拟。
| {{htmlJSON.Style}} | SimpleCalculation |
| {{htmlJSON.Categories}} | Hydrosphere / Earth System Subject |
| {{htmlJSON.Language}} | EN_US | |
| {{htmlJSON.Name}} | GWSiB | |
| {{htmlJSON.Keywords}} | Coupling,AquiferFlow,SiB2 | |
| {{htmlJSON.Abstract}} | Coupling a groundwater model with a land surface model to improve water and energy cycle simulation | |
| {{htmlJSON.Type}} | {{htmlJSON.Property}} | {{htmlJSON.Value}} |
|---|---|---|
| {{htmlJSON.HardwareConfigures}} | cpu core numble | [1,infinite) |
| memory size | [1GB,infinite) | |
| {{htmlJSON.SoftwareConfigures}} | Operating System | win 6||win 7||win 8||win 8.1||win 10||win xp |
实现了一个典型的陆面过程模型 SiB2 和 地下水三维动力学模型AquiferFlow 的耦合，增强了陆面过程中地下水过程的模拟，提高了陆表能水过程的模拟能力。
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