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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. When a small water parcel is…
Internal tides, internal mixing, and biological enhancement, Simple explanation & Propagation and dissipation
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internal tides tide surface ocean wave waves mixing energy water topography circulation may deep generated near interior gravity midocean tidal
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| the Hawaiian Ridge | instance of | midocean topography | 0.80 | text |
| Tahiti | instance of | midocean topography | 0.80 | text |
| the Macquarie Ridge | instance of | midocean topography | 0.80 | text |
| and submarine ridges in the Luzon Strait | instance of | midocean topography | 0.80 | text |
| the Australian North West Shelf also generate large internal tides | instance of | Continental slopes | 0.80 | text |
| Internal tide | related to Abyssal mixing and meridional overturning circulation | The | 0.60 | section |
| Internal tide | related to Abyssal mixing and meridional overturning circulation | If | 0.60 | section |
| Internal tide | related to Abyssal mixing and meridional overturning circulation | While | 0.60 | section |
| Internal tide | related to Abyssal mixing and meridional overturning circulation | PW | 0.60 | section |
| Internal tide | related to Abyssal mixing and meridional overturning circulation | TW | 0.60 | section |
| Internal tide | related to Abyssal mixing and meridional overturning circulation | Sandstrom | 0.60 | section |
| Internal tide | related to Abyssal mixing and meridional overturning circulation | Most | 0.60 | section |
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