Research news on ocean tide

Ocean tide is a periodic sea-level oscillation driven primarily by the gravitational forces of the Moon and Sun acting on Earth’s oceans, modulated by Earth’s rotation and the configuration of ocean basins. It manifests as propagating tidal waves with characteristic constituents (e.g., M2, S2, K1) describable by harmonic analysis. Tidal dynamics are governed by the shallow-water equations on a rotating sphere, incorporating Coriolis effects, coastal and seafloor topography, and resonance within semi-enclosed basins. Ocean tides play a fundamental role in coastal hydrodynamics, mixing, sediment transport, and energy dissipation in the Earth–Moon system.

Human-altered estuaries now drive stronger tides farther inland

A study led by Wageningen University & Research shows that human interventions have significantly changed tides in river estuaries over the past centuries. In many regions around the world, the difference between high and ...

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