Page 3: Research news on tides (oceanic)

Oceanic tides are periodic sea-level oscillations driven primarily by the gravitational forces of the Moon and Sun and the Earth’s rotation, expressed as propagating long waves in the ocean basins. They are described as equilibrium and dynamic tides, with the latter governed by the Laplace tidal equations that incorporate Coriolis effects, bathymetry, and basin geometry. Tides are decomposed into harmonic constituents (e.g., M2, S2, K1), each with distinct frequencies and phases, enabling precise tidal prediction. They play critical roles in coastal dynamics, mixing, and energy dissipation, and are significant for processes such as sediment transport and ocean circulation.

Flood prediction could boost road resilience off Georgia's coast

Communities on small islands are on the front lines of worsening flood risks—not just from severe storms but from persistent tidal flooding events. Scientists estimate that within 15 years, high-tide flood events could triple ...

Swarm detects ocean tides' magnetic signatures

A study using data from ESA's Swarm mission suggests that faint magnetic signatures created by Earth's tides can help us determine magma distribution under the seabed and could even give us insights into long-term trends ...

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