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The geoid (/ˈdʒiː.ɔɪd/ JEE-oyd) is the shape that the ocean surface would take under the influence of the gravity of Earth, including gravitational attraction and Earth's rotation, if other influences such as winds and tides were absent. This surface is extended through the continents (such as might be approximated with very narrow hypothetical canals).…
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| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Geoid | is a | particular equipotential surface | 0.90 | text |
| winds | instance of | if other influences | 0.80 | text |
| tides were absent | instance of | if other influences | 0.80 | text |
| ocean tides | instance of | the discrepancy is due to other factors | 0.80 | text |
| atmospheric pressure | instance of | the discrepancy is due to other factors | 0.80 | text |
| GOCE | instance of | and lately from satellite gravity missions | 0.80 | text |
| GRACE | instance of | and lately from satellite gravity missions | 0.80 | text |
| Geoid | related to Description | The | 0.60 | section |
| Geoid | related to Description | Earth | 0.60 | section |
| Geoid | related to Description | Earth's | 0.60 | section |
| Geoid | related to Description | Although | 0.60 | section |
| Geoid | related to Description | Mount Everest | 0.60 | section |
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