Energy-containing eddies: Difference between revisions
From Glossary of Meteorology
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<div class="definition"><div class="short_definition">A [[range]] of [[eddy]] sizes containing much of the [[energy]] in the [[turbulence spectrum]].</div><br/> <div class="paragraph">Approximately centered on [[integral length scales]], these eddies are larger than those in the [[inertial subrange]] and smaller than the semipermanent eddies associated with the spectrum's formation. <br/>''See'' [[turbulence length scales]].</div><br/> </div> | <div class="definition"><div class="short_definition">A [[range]] of [[eddy]] sizes containing much of the [[energy]] in the [[turbulence spectrum|turbulence spectrum]].</div><br/> <div class="paragraph">Approximately centered on [[integral length scales]], these eddies are larger than those in the [[inertial subrange]] and smaller than the semipermanent eddies associated with the spectrum's formation. <br/>''See'' [[turbulence length scales]].</div><br/> </div> | ||
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Latest revision as of 15:54, 25 April 2012
energy-containing eddies
Approximately centered on integral length scales, these eddies are larger than those in the inertial subrange and smaller than the semipermanent eddies associated with the spectrum's formation.
See turbulence length scales.
See turbulence length scales.
