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  2. Ocean general circulation model - Wikipedia

    en.wikipedia.org/wiki/Ocean_general_circulation...

    The first generation of OGCMs assumed “rigid lid” to eliminate high-speed external gravity waves. According to CFL criteria without those fast waves, we can use a bigger time step, which is not so computationally expensive. But it also filtered those ocean tides and other waves having the speed of tsunamis.

  3. Marine geophysics - Wikipedia

    en.wikipedia.org/wiki/Marine_geophysics

    Marine gravity profiles made across Mid-Ocean Ridges showed a lack of a gravity anomaly, the Free-air anomaly is small or near zero when averaged over a broad area. [ 36 ] [ 37 ] This suggested that although ridges reached a height at their crest of two kilometers or more above the deep ocean basins, that extra mass was not related to an ...

  4. Internal tide - Wikipedia

    en.wikipedia.org/wiki/Internal_tide

    The interfacial movement between two layers of ocean is large compared to surface movement because although as with surface waves, the restoring force for internal waves and tides is still gravity, its effect is reduced because the densities of the two layers are relatively similar compared to the large density difference at the air-sea interface.

  5. Origin of mysterious giant ‘gravity hole’ in Indian Ocean ...

    www.aol.com/origin-mysterious-giant-gravity-hole...

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  6. Internal wave - Wikipedia

    en.wikipedia.org/wiki/Internal_wave

    The displacement of the thermocline of a lake, which separates warmer surface from cooler deep water, feels the buoyancy force expressed through the reduced gravity. For example, the density difference between ice water and room temperature water is 0.002 the characteristic density of water. So the reduced gravity is 0.2% that of gravity.

  7. Dead zones recorded in Atlantic Ocean for first time - AOL

    www.aol.com/article/2015/05/04/dead-zones...

    The Atlantic Ocean is teeming with life, but for the first time researchers have discovered dead zones in these waters - areas low in both oxygen and salinity - off the coast of Africa. Fish can't ...

  8. Free-air gravity anomaly - Wikipedia

    en.wikipedia.org/wiki/Free-air_gravity_anomaly

    Over the ocean where gravity is measured from ships near sea level, there is no or little free-air correction. In marine gravity surveys, it was observed that the free-air anomaly is positive but very small over the Mid-Ocean Ridges in spite of the fact that these features rise several kilometers above the surrounding seafloor. [6]

  9. Infragravity wave - Wikipedia

    en.wikipedia.org/wiki/Infragravity_wave

    Infragravity waves are surface gravity waves with frequencies lower than the wind waves – consisting of both wind sea and swell – thus corresponding with the part of the wave spectrum lower than the frequencies directly generated by forcing through the wind. Infragravity waves are ocean surface gravity waves generated by ocean waves of ...