K-ε closure: Difference between revisions
From Glossary of Meteorology
(Created page with " {{TermHeader}} {{TermSearch}} <div class="termentry"> <div class="term"> == ''k''–ε closure == </div> <div class="definition"><div class="short_definitio...") |
m (Rewrite with Template:Term and clean up) |
||
(One intermediate revision by the same user not shown) | |||
Line 1: | Line 1: | ||
{{Term | |||
|Display title=''k''–ε closure | |||
{{ | |Definitions={{Definition | ||
|Num=1 | |||
|Meaning=A type of one-and-a-half-order [[turbulence closure]] that retains forecast equations for mean (first-order [[statistics]]) variables such as [[potential temperature]] and [[wind]] components, and also retains equations for [[variances]] ([[turbulence kinetic energy]] and [[temperature]] variance, symbolized by ''k'') and for [[molecular dissipation]] or destruction of variances (symbolized by ε). | |||
|Explanation=<br/>''Compare'' [[first-order closure]], [[K-theory]], [[second-order closure]], [[nonlocal closure]], [[Reynolds averaging|Reynolds averaging]], [[closure assumptions]]. | |||
}} | |||
}} | |||
Latest revision as of 11:59, 26 March 2024
A type of one-and-a-half-order turbulence closure that retains forecast equations for mean (first-order statistics) variables such as potential temperature and wind components, and also retains equations for variances (turbulence kinetic energy and temperature variance, symbolized by k) and for molecular dissipation or destruction of variances (symbolized by ε).