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An antidune is a bedform found in fluvial and other channeled environments. Antidunes occur in supercritical flow, meaning that the Froude number is greater than 1.0 or the flow velocity exceeds the wave velocity; this is also known as upper flow regime. In antidunes, sediment is deposited on the upstream (stoss) side and eroded from the downstream (lee)…
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antidunes flow regime upstream migrate wave bedforms bedform downstream amplitude also surface velocity trough crest environments froude upper water supercritical
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Antidune | is a | bedform found in fluvial and other channeled environments | 0.90 | text |
| Antidune | related to Formation | Antidunes | 0.60 | section |
| Antidune | related to Formation | Unlike | 0.60 | section |
| Antidune | related to Formation | When | 0.60 | section |
| Antidune | related to Formation | Flume | 0.60 | section |
| Antidune | related to Formation | While | 0.60 | section |
| Antidune | related to Formation | If | 0.60 | section |
| Antidune | related to Formation | Froude | 0.60 | section |
| Antidune | related to history | In | 0.60 | section |
| Antidune | related to history | Vaughan Cornish | 0.60 | section |
| Antidune | related to history | Royal Geographical Society | 0.60 | section |
| Antidune | related to history | He | 0.60 | section |
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