A common misconception suggests that differing sea levels between the Pacific and Atlantic Oceans would impede maritime travel. The reality? The difference averages a mere 20 centimeters (8 inches)—negligible for any vessel.
Ships float on water, not on the ocean floor. Their draft (depth below waterline) is measured from the surface, so a slight variation in absolute sea level between oceans is irrelevant to buoyancy or propulsion. The Panama Canal, which connects the two oceans, uses a lock system to raise and lower ships across the continental divide—not because of a sea-level mismatch, but because the terrain itself rises.
Only in port operations does local sea level become critical. Extreme low tides can ground deep-draft vessels; storm surges can prevent departure. But these are temporary, localized conditions—not inherent oceanic differences.
The world's oceans form a single, interconnected body of water. Ships traverse them freely, their routes determined by currents, weather, and geography—not by a few centimeters of sea-level variance.