“…This assumption is reasonable for the rainfall intensity in a small area, but it is not realistic for the recharge of aquifers, because the process of infiltration is affected by geological characteristics such as topography, soil type and evapotranspiration, land use type, and human activities (Park et al., 2014; Werner et al., 2017). Field investigations have showed that the groundwater lens shape and thickness can be affected by spatially variable recharge rates induced by ridge topography (Ruppel et al., 2000), terrain and vegetation patterns (Schneider & Kruse, 2003, 2006), distribution of different soil types (Park et al., 2014) and heterogeneous hydrogeological properties including hydraulic conductivity, impermeable layer, and boundary conditions (Cellone et al., 2018; Holt et al., 2019; Rathore et al., 2018; Rathore, Lu & Luo, 2020; Sheng et al., 2020). In addition, the knowledge and insights on how the volume and shape of a groundwater lens change in response to spatially variable recharge rates can provide very useful information for determining the location and recharge rate of artificial recharge to control seawater intrusion (Bouwer, 2002; Rajasekhar et al., 2019; Senanayake et al., 2016).…”