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In atmospheric dynamics, oceanography, asteroseismology and geophysics, the Brunt–Väisälä frequency, or buoyancy frequency, is a measure of the stability of a fluid to vertical displacements such as those caused by convection. More precisely it is the frequency at which a vertically displaced parcel will oscillate within a statically stable environment.…
In meteorology and astrophysics, Derivation for a general fluid & In oceanography
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displaystyle parcel density brunt väisälä frequency gas rho frac vertical stratification fluid height acceleration atmospheric convection positive pressure equiv dz
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| those caused by convection | instance of | is a measure of the stability of a fluid to vertical displacements | 0.80 | text |
| Brunt–Väisälä frequency | related to Context | The | 0.60 | section |
| Brunt–Väisälä frequency | related to Context | Newton's | 0.60 | section |
| Brunt–Väisälä frequency | related to Context | If | 0.60 | section |
| Brunt–Väisälä frequency | related to Context | In | 0.60 | section |
| Brunt–Väisälä frequency | related to Context | N2 | 0.60 | section |
| Brunt–Väisälä frequency | related to Context | The Brunt | 0.60 | section |
| Brunt–Väisälä frequency | related to Context | Väisälä | 0.60 | section |
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