Stability Through Cycling
Subduction shows that water *does* leave the ocean basin, but it doesn't drain into a void. Instead, it is temporarily stored in the Earth's interior as part of a slow geological cycle. Because this process takes millions of years and involves chemical binding rather than rapid fluid loss, the oceans remain stable and full on human timescales. The Earth is a closed system for water, constantly recycling it between the surface and the deep interior.
Timescale Matters
Unlike a bathtub drain which empties in minutes, the subduction cycle operates over millions of years. This vast timescale ensures that the volume of water entering the mantle is balanced by water returning via volcanism and precipitation.