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  2. Ocean current - Wikipedia

    en.wikipedia.org/wiki/Ocean_current

    Ocean surface currents Distinctive white lines trace the flow of surface currents around the world. Visualization showing global ocean currents from January 1, 2010, to December 31, 2012, at sea level, then at 2,000 m (6,600 ft) below sea level Animation of circulation around ice shelves of Antarctica

  3. Internal tide - Wikipedia

    en.wikipedia.org/wiki/Internal_tide

    Internal tides are generated as the surface tides move stratified water up and down sloping topography, which produces a wave in the ocean interior. So internal tides are internal waves at a tidal frequency. The other major source of internal waves is the wind which produces internal waves near the inertial frequency.

  4. Bathymetry - Wikipedia

    en.wikipedia.org/wiki/Bathymetry

    The beams update many times per second (typically 0.1–50 Hz depending on water depth), allowing faster boat speed while maintaining 100% coverage of the seafloor. Attitude sensors allow for the correction of the boat's roll and pitch on the ocean surface, and a gyrocompass provides accurate heading information to correct for vessel yaw. (Most ...

  5. Nasa shares chilling animation showing how far sea level has ...

    www.aol.com/nasa-shares-chilling-animation...

    A chilling animation from Nasa shows how far the sea level has risen in the past 30 years.. In the visualisation, the average level rises by over 10cm between 1993 and 2022. “As the planet warms ...

  6. Ship motions - Wikipedia

    en.wikipedia.org/wiki/Ship_motions

    This motion is generated directly either by the water and wind motion, particularly lateral wave motion, exerting forces against the hull or by the ship's own propulsion; or indirectly by the inertia of the ship while turning. This movement can be compared to the vessel's lateral drift from its course.

  7. Geostrophic current - Wikipedia

    en.wikipedia.org/wiki/Geostrophic_current

    The force pushing the water towards the low pressure region is called the pressure gradient force. In a geostrophic flow, instead of water moving from a region of high pressure (or high sea level) to a region of low pressure (or low sea level), it moves along the lines of equal pressure . This occurs because the Earth is rotating. The rotation ...

  8. Mooring (oceanography) - Wikipedia

    en.wikipedia.org/wiki/Mooring_(oceanography)

    The mooring is held up in the water column with various forms of buoyancy such as glass balls and syntactic foam floats. The attached instrumentation is wide-ranging but often includes CTDs (conductivity, temperature depth sensors), current meters (e.g. acoustic Doppler current profilers or deprecated rotor current meters), and biological sensors to measure various parameters.

  9. Physical oceanography - Wikipedia

    en.wikipedia.org/wiki/Physical_oceanography

    Perspective view of the sea floor of the Atlantic Ocean and the Caribbean Sea. The purple sea floor at the center of the view is the Puerto Rico Trench.. Roughly 97% of the planet's water is in its oceans, and the oceans are the source of the vast majority of water vapor that condenses in the atmosphere and falls as rain or snow on the continents.