Step 1: Picture the coastal aquifer balance.
Near a coastline, fresh groundwater and seawater sit side by side underground, held in place by the outward push of fresh water pressure.
Step 2: Think about what upsets that balance.
If wells draw out more water than natural recharge can replace, the freshwater head drops and its outward push weakens.
Step 3: See the result.
With less freshwater pressure holding it back, seawater moves inland into the aquifer, causing intrusion, unlike the other options which would actually strengthen the freshwater side.
\[ \boxed{\text{Pumping exceeds recharge}} \]