Figure 2.

Numerical model results for the change in groundwater level ∆h t at different distances from the coastline for SLR Scenario 1 and for (a) fixed‐head inland boundary condition and (b) fixed‐flux inland boundary condition.

Numerical model results for the change in groundwater level ∆h t at different distances from the coastline for SLR Scenario 1 and for (a) fixed‐head inland boundary condition and (b) fixed‐flux inland boundary condition.