2001
DOI: 10.1016/s1620-7742(01)01338-1
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Naissance des corrélations triples de vorticité dans une turbulence statistiquement homogène soumise à une rotation

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Cited by 18 publications
(21 citation statements)
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“…This second structure (best seen in figure 12(b)) is fluctuating strongly having more small scales. The persistence of corotating structures in rotating turbulence has been observed in experiments (Hopfinger et al 1982;Morize et al 2005;Gallet et al 2014) and has been discussed in various works (Hopfinger & van Heijst 1993;Bartello et al 1994;Gence & Frick 2001;Sreenivasan & Davidson 2008;Staplehurst et al 2008;Gallet et al 2014). Perhaps it is not surprising that structures with vorticity anti-aligned to rotation are more responsive to 3D perturbations.…”
Section: Intermittent Burstsmentioning
confidence: 86%
“…This second structure (best seen in figure 12(b)) is fluctuating strongly having more small scales. The persistence of corotating structures in rotating turbulence has been observed in experiments (Hopfinger et al 1982;Morize et al 2005;Gallet et al 2014) and has been discussed in various works (Hopfinger & van Heijst 1993;Bartello et al 1994;Gence & Frick 2001;Sreenivasan & Davidson 2008;Staplehurst et al 2008;Gallet et al 2014). Perhaps it is not surprising that structures with vorticity anti-aligned to rotation are more responsive to 3D perturbations.…”
Section: Intermittent Burstsmentioning
confidence: 86%
“…There are, however, other possible explanations for the asymmetry. For example, Gence & Frick (2001) considered fully developed, isotropic turbulence which is suddenly subjected Figure 18. Probability density function of the axial vorticity, ω z : -, initial distribution;…”
Section: Statistics In a Horizontal Planementioning
confidence: 99%
“…In particular, it has been shown that the cyclones and anticyclones have different stability properties [31] and different probabilities to be generated at finite Rossby number [33]. Moreover, the correlations between the strain tensor and the vorticity in isotropic turbulence can be responsible for the development of a positive skewness of vertical vorticity when the flow is suddenly subjected to rotation [34]. Interestingly, a similar asymmetry has been observed also in the tropopause [35] and in the stratosphere [36], even though the physical mechanisms acting in the atmosphere are more complex than in idealized rotating turbulence.…”
Section: Introductionmentioning
confidence: 99%