Reconstruction of groundwater-induced gravity effects using a physical hydrological model at Lhasa Station, Tibetan Plateau

Key Points

• Gravity effects induced by groundwater changes were successfully reconstructed using a physical hydrological model.
• This analysis highlights significant variations in gravity, particularly during wet seasons, indicating groundwater movement.
• The method employed allows for precise elucidation of the relationship between groundwater and gravity effects over time.
• Findings support improved understanding of groundwater dynamics, crucial for managing water resources in the Tibetan Plateau.