2004
DOI: 10.1023/b:boun.0000039373.45669.68
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Richardson's Law in Large-Eddy Simulations of Boundary-Layer Flows

Abstract: Relative dispersion in a neutrally stratified planetary boundary layer (PBL) is investigated by means of Large-Eddy Simulations (LES). Despite the small extension of the inertial range of scales in the simulated PBL, our Lagrangian statistics turns out to be compatible with the Richardson t 3 law for the average of square particle separation. This emerges from the application of nonstandard methods of analysis through which a precise measure of the Richardson constant was also possible. Its values is estimated… Show more

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Cited by 20 publications
(19 citation statements)
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“…We see that a collapse of curves is beginning to form for all initial separations. We estimate the value of g to be approximately 0.50± 0.05, which agrees with the value computed above and with previous estimates of g. 13,14,29 This method has the advantage of relative insensitivity to the initial separation and avoids the problem of the nonzero intercept discussed in Sec. III A.…”
Section: ͗T ͑Rsupporting
confidence: 89%
“…We see that a collapse of curves is beginning to form for all initial separations. We estimate the value of g to be approximately 0.50± 0.05, which agrees with the value computed above and with previous estimates of g. 13,14,29 This method has the advantage of relative insensitivity to the initial separation and avoids the problem of the nonzero intercept discussed in Sec. III A.…”
Section: ͗T ͑Rsupporting
confidence: 89%
“…This new method has been already exploited for studies of relative dispersion in atmospheric and oceanic systems , Joseph and Legras 2002, Boffetta et al 2001, LaCasce and Ohlmann 2003, Gioia et al 2003 and also in laboratory convection experiments (Boffetta et al 2000b). …”
Section: Introductionmentioning
confidence: 99%
“…Recent experimental and numerical studies agree about a value of the Richardson's constant C R 5 · 10 −1 (Ott and Mann, 2002, Boffetta and Sokolov, 2002, Gioia et al, 2004. The Richardson's law (II.3) can be derived from the fundamental assumption of the theory of turbulence stating that |∆ V (δ)| 2 ∼ δ 2/3 inside the inertial range (Frisch, 1995).…”
Section: Main Aspects Of Lagrangian Dispersionmentioning
confidence: 95%
“…The Richardson's law (II.3) can be derived from the fundamental assumption of the theory of turbulence stating that |∆ V (δ)| 2 ∼ δ 2/3 inside the inertial range (Frisch, 1995). It can be verified, by a simple dimensional argument, that the equivalent of (II.3) in terms of FSLE is λ(δ) = αδ −2/3 , where α 3 is a quantity of the same order as (Gioia et al, 2004, Lacorata et al, 2004.…”
Section: Main Aspects Of Lagrangian Dispersionmentioning
confidence: 99%
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