1978
DOI: 10.1017/s002211207800227x
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Models of the scalar spectrum for turbulent advection

Abstract: Several models are developed for the high-wavenumber portion of the spectral transfer function of scalar quantities advected by high-Reynolds-number, locally isotropic turbulent flow. These models are applicable for arbitrary Prandtl or Schmidt number, v/D, and the resultant scalar spectra are compared with several experiments having different v/D. The ‘bump’ in the temperature spectrum of air observed over land is shown to be due to a tendency toward a viscous-convective range and the presence of this bump is… Show more

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Cited by 290 publications
(165 citation statements)
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“…But an anomalous k-1 subrange is also observed experimentally for Prandtl number as low as 0.7, the atmospheric value (the "bump" , Hill 1978). Therefore, even at Pr = 1 truncation, as indicated by the scalar-derivative flatness, becomes important for R).. > 18 on a 32 3 grid.…”
Section: Jmentioning
confidence: 70%
“…But an anomalous k-1 subrange is also observed experimentally for Prandtl number as low as 0.7, the atmospheric value (the "bump" , Hill 1978). Therefore, even at Pr = 1 truncation, as indicated by the scalar-derivative flatness, becomes important for R).. > 18 on a 32 3 grid.…”
Section: Jmentioning
confidence: 70%
“…(3) Here the structure parameter C 2 n depends in general on the temperature gradient on the scales larger than L 0 . See, e.g., [22], [16] and [4] for more sophisticated models of turbulent refractive index fields.…”
Section: Introductionmentioning
confidence: 99%
“…to the more realistic atmospheric spectrum developed by Hill, (Hill, 1978) and defined analytically by Andrews (Andrews, 1998) …”
Section: Beam-propagation Simulationsmentioning
confidence: 99%