Ocean warming is causing subtle changes in tides.
• Warmth increases energy transfer from tides with larger vertical movement (barotropic) to tides with smaller vertical movement (baroclinic).
• This results in open-ocean tides losing a few percent more energy to internal waves compared to three decades ago.
• The observed changes in surface tides are small (about a 1-centimeter drop in coastal tide levels over several decades).
• However, even minor tidal changes can have significant impacts on areas with complex underwater topography and pronounced tidal activity (e.g., Gulf of Maine, northern Australia).


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