Page 2: 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.

Sea level rise threatens the North Sea coast more than expected

As a result of climate change, rising sea levels are threatening low-lying coastal areas around the world, such as the Wadden Sea in the North Sea. Tidal basins form a natural protective barrier there. They connect the mainland ...

Regional ocean dynamics can be better emulated with AI models

The Gulf of Mexico, a regional ocean, is hugged by the southeastern United States and a large stretch of the Mexican coast, making it very important for both countries. The area helps bring goods to local and global markets, ...

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