The ocean conducts electricity—but it's a mediocre conductor compared to metals, and its conductivity varies dramatically with conditions.
Metals conduct via free electrons. Seawater conducts via dissolved ions—primarily Na⁺ and Cl⁻ from salt (NaCl), plus Mg²⁺, SO₄²⁻, Ca²⁺, K⁺, and others. These charged particles migrate in an electric field, creating current.
Higher salinity = more ions = higher conductivity. Open ocean (~35 PSU): ~5 S/m. Estuaries: variable. Hypersaline lagoons: up to 7 S/m. Freshwater: 0.005-0.05 S/m.
Warmer water = lower viscosity = higher ion mobility = higher conductivity. ~2% increase per °C. Tropical surface water conducts better than polar deep water.
Minor effect. Increased pressure slightly reduces ion mobility, but temperature and salinity dominate.
Marine organisms affect local conductivity:
CTD (Conductivity-Temperature-Depth) profilers measure conductivity to derive salinity—fundamental oceanographic data. Autonomous gliders and Argo floats provide global coverage.
Seawater's ionic conductivity enables unique applications (seawater batteries, mineral extraction) but remains fundamentally limited compared to electronic conduction. It's a conductor by chemistry, not by engineering merit.