Buoyancy flux: Difference between revisions

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The vertical [[kinematic flux]] of [[virtual potential temperature]] [[File:ams2001glos-Bex04.gif|link=|ams2001glos-Bex04]], which when  multiplied by the [[buoyancy]] parameter (''g''/''T''<sub>''v''</sub>) yields a [[flux]] that is proportional to buoyancy, that  is,    <blockquote>[[File:ams2001glos-Be25.gif|link=|center|ams2001glos-Be25]]</blockquote>  <br/>This is also a term in the [[turbulence kinetic energy]] budget, describing buoyant production  or [[consumption]] of [[turbulence]]. It also appears in the numerator of the [[flux Richardson number]].<br/> Stull, R. B. 1988. An Introduction to Boundary Layer Meteorology. 666 pp.  
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== buoyancy flux ==
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<div class="definition"><div class="short_definition">The vertical [[kinematic flux]] of [[virtual potential temperature]] <div class="inline-formula">[[File:ams2001glos-Bex04.gif|link=|ams2001glos-Bex04]]</div>, which when  multiplied by the [[buoyancy]] parameter (''g''/''T''<sub>''v''</sub>) yields a [[flux]] that is proportional to buoyancy, that  is,    <div class="display-formula"><blockquote>[[File:ams2001glos-Be25.gif|link=|center|ams2001glos-Be25]]</blockquote></div>  </div><br/><div class="paragraph">This is also a term in the [[turbulence kinetic energy]] budget, describing buoyant production  or [[consumption]] of [[turbulence]]. It also appears in the numerator of the [[flux Richardson number]].</div><br/> </div><div class="reference">Stull, R. B. 1988. An Introduction to Boundary Layer Meteorology. 666 pp. </div><br/>
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Latest revision as of 23:22, 13 January 2024

The vertical kinematic flux of virtual potential temperature ams2001glos-Bex04, which when multiplied by the buoyancy parameter (g/Tv) yields a flux that is proportional to buoyancy, that is,
ams2001glos-Be25

This is also a term in the turbulence kinetic energy budget, describing buoyant production or consumption of turbulence. It also appears in the numerator of the flux Richardson number.
Stull, R. B. 1988. An Introduction to Boundary Layer Meteorology. 666 pp.


  1. That property of an object that enables it to float on the surface of a liquid, or ascend through and remain freely suspended in a compressible fluid such as the atmosphere.
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