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Jan Kleissl Department of Geography and Environmental Engineering, and Center for Environmental and Applied Fluid Dynamics, The Johns Hopkins University, Baltimore, Maryland

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Marc B. Parlange Department of Geography and Environmental Engineering, and Center for Environmental and Applied Fluid Dynamics, The Johns Hopkins University, Baltimore, Maryland

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Charles Meneveau Department of Mechanical Engineering, and Center for Environmental and Applied Fluid Dynamics, The Johns Hopkins University, Baltimore, Maryland

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Corresponding author address: Charles Meneveau, JHU, 3400 N. Charles St., Baltimore, MD 21218-2681 Email: meneveau@jhu.edu

Corresponding author address: Charles Meneveau, JHU, 3400 N. Charles St., Baltimore, MD 21218-2681 Email: meneveau@jhu.edu

Because of a production error, Figs. 2, 5, and 10 in Kleissl et al. (2004) appeared in black and white instead of in color. The color figures that should have appeared are reproduced below.

REFERENCES

Kleissl, J., M. B. Parlange, and C. Meneveau, 2004: Field experimental study of dynamic Smagorinsky models in the atmospheric surface layer. J. Atmos. Sci., 61 , 2296–2307.

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Fig. 2.
Fig. 2.

Contour plots of conditional PDF of (csΔ,emp)2, P(cs2|Δ/L), for array 2 (Δ/z ∼ 1.1). The contours show log10 P(cs2|Δ/L). The averaging time to compute cs(Δ) is Tc = 3.2 s ∼ 2.0Δ/<u>. The solid line is the empirical fit of Eq. (14). The dashed line shows (csΔ)2 = 0.

Citation: Journal of the Atmospheric Sciences 62, 1; 10.1175/JAS-V62N1A05.1

Fig. 5.
Fig. 5.

Contour plots of the PDF of (csΔ,dyn)2 conditioned on Δ/L for array 2 (Δ/z ∼ 1.1). The contours show log10 P(cs2|Δ/L). The averaging time to compute cs(Δ) is Tc = 3.2 s ∼ 2.0Δ/<u>. The solid line is the empirical fit of Eq. (14). The dashed line shows (csΔ)2 = 0.

Citation: Journal of the Atmospheric Sciences 62, 1; 10.1175/JAS-V62N1A05.1

Fig. 10.
Fig. 10.

Contour plots of conditional PDF of (a) β and (b) (cs(Δ,sd-dyn))2 from the scale-dependent dynamic model. The contours show (a) log10 P(β|Δ/L) and (b) log10 P(cs2|Δ/L). The averaging time to compute cs(Δ) is Tc = 3.2 s ∼ 2.0Δ/<u>. The dashed line in (a) shows β = 0.327 [cf. Eq. (15)]. The dashed and solid lines in (b) show (csΔ)2 = 0 and the empirical fit of Eq. (14), respectively.

Citation: Journal of the Atmospheric Sciences 62, 1; 10.1175/JAS-V62N1A05.1

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  • Kleissl, J., M. B. Parlange, and C. Meneveau, 2004: Field experimental study of dynamic Smagorinsky models in the atmospheric surface layer. J. Atmos. Sci., 61 , 2296–2307.

    • Search Google Scholar
    • Export Citation
  • Fig. 2.

    Contour plots of conditional PDF of (csΔ,emp)2, P(cs2|Δ/L), for array 2 (Δ/z ∼ 1.1). The contours show log10 P(cs2|Δ/L). The averaging time to compute cs(Δ) is Tc = 3.2 s ∼ 2.0Δ/<u>. The solid line is the empirical fit of Eq. (14). The dashed line shows (csΔ)2 = 0.

  • Fig. 5.

    Contour plots of the PDF of (csΔ,dyn)2 conditioned on Δ/L for array 2 (Δ/z ∼ 1.1). The contours show log10 P(cs2|Δ/L). The averaging time to compute cs(Δ) is Tc = 3.2 s ∼ 2.0Δ/<u>. The solid line is the empirical fit of Eq. (14). The dashed line shows (csΔ)2 = 0.

  • Fig. 10.

    Contour plots of conditional PDF of (a) β and (b) (cs(Δ,sd-dyn))2 from the scale-dependent dynamic model. The contours show (a) log10 P(β|Δ/L) and (b) log10 P(cs2|Δ/L). The averaging time to compute cs(Δ) is Tc = 3.2 s ∼ 2.0Δ/<u>. The dashed line in (a) shows β = 0.327 [cf. Eq. (15)]. The dashed and solid lines in (b) show (csΔ)2 = 0 and the empirical fit of Eq. (14), respectively.

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