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Vertical Profiles of Turbulence Parameters in the Thermal Internal Boundary Layer

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Abstract

The correct simulation of pollutant dispersion in coastal regions demands understanding the turbulence structure of the thermal internal boundary layer (TIBL), which typically occurs in daytime when maritime air is advected over the continent. Such a structure is investigated using 10 levels of turbulence observations made at a 140-m micrometeorological mast installed at 3500 m from the shoreline in south-eastern Brazil, with TIBL dimensionless vertical profiles of the turbulence parameters commonly used in Lagrangian and Eulerian dispersion models determined. To accomplish that, the TIBL height \(z_i\) is estimated using a vertical-flux-convergence approach, developed here. The values experimentally obtained for \(z_i\) agree with those predicted by a widely-used model for TIBL growth. In general, the normalized turbulent profiles evaluated for the TIBL differ from those previously obtained in the convective boundary layer (CBL). The horizontal eddy diffusivities evaluated for the TIBL are larger than those typically observed in the CBL, while the vertical ones are similar for both boundary layers. Finally, it is shown that CBL similarity relationships can be used to describe turbulent parameters as long as the proper empirical constants are used.

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References

  • Acevedo OC, Degrazia GA, Puhales FS, Martins LG, Oliveira PE, Teichrieb C, Silva SM, Maroneze R, Bodmann B, Mortarini L, Cava D, Anfossi D (2018) Monitoring the micrometeorology of a coastal site next to a thermal power plant from the surface to 140 m. Bull Am Meteorol Soc 99(4):725–738

    Article  Google Scholar 

  • Bevington PR, Robinson DK (2003) Data reduction and error analysis. McGraw Hill, New York

    Google Scholar 

  • Brost RA, Haagenson PL, Kuo YH (1988) The effect of diffusion on tracer puffs simulated by a regional scale Eulerian model. J Geophys Res Atmos 93(D3):2389–2404

    Article  Google Scholar 

  • Carson D (1973) The development of a dry inversion-capped convectively unstable boundary layer. Q J R Meteorol Soc 99(421):450–467

    Article  Google Scholar 

  • Caughey S, Palmer S (1979) Some aspects of turbulence structure through the depth of the convective boundary layer. Q J R Meteorol Soc 105(446):811–827

    Article  Google Scholar 

  • De Baas AF, Van Dop H, Nieuwstadt FT (1986) An application of the Langevin equation for inhomogeneous conditions to dispersion in a convective boundary layer. Q J R Meteorol Soc 112(471):165–180

    Article  Google Scholar 

  • Deardorff J, Willis G (1975) A parameterization of diffusion into the mixed layer. J Appl Meteorol Climatol 14(8):1451–1458

    Article  Google Scholar 

  • Deardorff J, Willis G (1985) Further results from a laboratory model of the convective planetary boundary layer. Boundary-Layer Meteorol 32(3):205–236

    Article  Google Scholar 

  • Degrazia G, Anfossi D (1998) Estimation of the Kolmogorov constant C\(_0\) from classical statistical diffusion theory. Atmos Environ 32(20):3611–3614

    Article  Google Scholar 

  • Degrazia GA, Moreira DM, Vilhena MT (2001) Derivation of an eddy diffusivity depending on source distance for vertically inhomogeneous turbulence in a convective boundary layer. J Appl Meteorol Climatol 40(7):1233–1240

    Article  Google Scholar 

  • Degrazia GA, Carvalho JC, Moreira DM, Vilhena MT, Roberti DR, Magalhães SG (2007) Derivation of a decorrelation timescale depending on source distance for inhomogeneous turbulence in a convective boundary layer. Phys A 374(1):55–65

    Article  Google Scholar 

  • Durand P, Druilhet A, Briere S (1989) A sea-land transition observed during the coast experiment. J Atmos Sci 46(1):96–116

    Article  Google Scholar 

  • Fedorovich E, Conzemius R, Mironov D (2004) Convective entrainment into a shear-free, linearly stratified atmosphere: bulk models reevaluated through large eddy simulations. J Atmos Sci 61(3):281–295

    Article  Google Scholar 

  • Frisch U (1995) Turbulence: the legacy of AN Kolmogorov. Cambridge University Press, Cambridge

    Book  Google Scholar 

  • Galmarini S, Attié J (2000) Turbulent transport atthe thermal internal boundary-layer top: wavelet analysis of aircraft measurements. Boundary-Layer Meteorol 94(2):175–196

    Article  Google Scholar 

  • Gamo M, Yamamoto S, Yokoyama O (1982) Airborne measurements of the free convective internal boundary layer during the sea breeze. J Meteorol Soc Jpn Ser II 60(6):1284–1298

    Article  Google Scholar 

  • Garratt J et al (1992) The atmospheric boundary layer. Cambridge University Press, Cambridge

    Google Scholar 

  • Gifford FA (1968) An outline of theories of diffusion in the lower layers of the atmosphere. Tech. Rep. TID-24190, Environmental Science Services Administration, Oak Ridge, Tenn

  • Gryning SE, Batchvarova E (1990) Analytical model for the growth of the coastal internal boundary layer during onshore flow. Q J R Meteorol Soc 116(491):187–203

    Article  Google Scholar 

  • Gryning SE, Batchvarova E, Brümmer B, Jørgensen H, Larsen S (2007) On the extension of the wind profile over homogeneous terrain beyond the surface boundary layer. Boundary-Layer Meteorol 124(2):251–268

    Article  Google Scholar 

  • Guillemet B, Isaka H, Mascart P (1983) Molecular dissipation of turbulent fluctuations in the convective mixed layer part I: height variations of dissipation rates. Boundary-Layer Meteorol 27(2):141–162

    Article  Google Scholar 

  • Hanna S, Chang J, Strimaitis D (1993) Hazardous gas model evaluation with field observations. Atmo Environ 27(15):2265–2285

    Article  Google Scholar 

  • Hanna SR (1981) Lagrangian and Eulerian time-scale relations in the daytime boundary layer. J Appl Meteorol Climatol 20(3):242–249

    Article  Google Scholar 

  • Hanna SR (1989) Confidence limits for air quality model evaluations, as estimated by bootstrap and jackknife resampling methods. Atmos Environ 23(6):1385–1398

    Article  Google Scholar 

  • Hara T, Ohya Y, Uchida T, Ohba R (2009) Wind-tunnel and numerical simulations of the coastal thermal internal boundary layer. Boundary-Layer Meteorol 130(3):365–381

    Article  Google Scholar 

  • Hicks B (1985) Behavior of turbulence statistics in the convective boundary layer. J Clim Appl Meteorol 24(6):607–614

    Article  Google Scholar 

  • Hinze J (1975) Turbulence. McGraw-Hill, New York

    Google Scholar 

  • Holtslag AA, Nieuwstadt FT (1986) Scaling the atmospheric boundary layer. Boundary-Layer Meteorol 36(1–2):201–209

    Article  Google Scholar 

  • Huang NE, Shen Z, Long SR, Wu MC, Shih HH, Zheng Q, Yen NC, Tung CC, Liu HH (1998) The empirical mode decomposition and the Hilbert spectrum for nonlinear and non-stationary time series analysis. Proc R Soc Lond A Mater 454(1971):903–995

    Article  Google Scholar 

  • Huang NE, Shen Z, Long SR (1999) A new view of nonlinear water waves: the Hilbert spectrum. Annu Rev Fluid Mech 31(1):417–457

    Article  Google Scholar 

  • Kaimal J, Wyngaard J, Izumi Y, Coté O (1972) Spectral characteristics of surface-layer turbulence. Q J R Meteorol Soc 98(417):563–589

    Article  Google Scholar 

  • Kaimal J, Wyngaard J, Haugen D, Coté O, Izumi Y, Caughey S, Readings C (1976) Turbulence structure in the convective boundary layer. J Atmos Sci 33(11):2152–2169

    Article  Google Scholar 

  • Kaimal JC, Finnigan JJ (1994) Atmospheric boundary layer flows. Oxford University Press, Oxford

    Book  Google Scholar 

  • Kim SW, Park SU, Moeng CH (2003) Entrainment processes in the convective boundary layer with varying wind shear. Bound-Layer Meteorol 108(2):221–45

  • Lamb R, Durran D (1978) Eddy diffusivities derived from a numerical model of the convective planetary boundary layer. Nuovo Cimento C 1(1):1–17

    Article  Google Scholar 

  • Lenschow D, Wyngaard JC, Pennell WT (1980) Mean-field and second-moment budgets in a baroclinic, convective boundary layer. J Atmos Sci 37(6):1313–1326

    Article  Google Scholar 

  • Lenschow DH (1974) Model of the height variation of the turbulence kinetic energy budget in the unstable planetary boundary layer. J Atmos Sci 31(2):465–474

    Article  Google Scholar 

  • Lenschow DH, Lothon M, Mayor SD, Sullivan PP, Canut G (2012) A comparison of higher-order vertical velocity moments in the convective boundary layer from lidar with in situ measurements and large-eddy simulation. Boundary-Layer Meteorol 143(1):107–123

    Article  Google Scholar 

  • Luhar AK, Britter RE (1989) A random walk model for dispersion in inhomogeneous turbulence in a convective boundary layer. Atmos Environ 23(9):1911–1924

    Article  Google Scholar 

  • Luhar AK, Sawford BL (1995) Lagrangian stochastic modeling of the coastal fumigation phenomenon. J Appl Meteorol Climatol 34(10):2259–2277

    Article  Google Scholar 

  • Martins LGN, Degrazia GA, Acevedo OC, Puhales FS, de Oliveira PE, Teichrieb CA, da Silva SM (2018) Quasi-experimental determination of turbulent dispersion parameters for different stability conditions from a tall micrometeorological tower. J Appl Meteorol Climatol 57(8):1729–1745

    Article  Google Scholar 

  • McRae GJ, Goodin WR, Seinfeld JH (1982) Development of a second-generation mathematical model for urban air pollution—I. Model formulation. Atmos Environ 16(4):679–696

    Article  Google Scholar 

  • Moeng CH, Wyngaard JC (1989) Evaluation of turbulent transport and dissipation closures in second-order modeling. J Atmos Sci 46(14):2311–2330

    Article  Google Scholar 

  • Panofsky HA, Dutton JA (1983) Atmospheric turbulence. Wiley, New York

    Google Scholar 

  • Raynor GS, Sethuraman S, Brown RM (1979) Formation and characteristics of coastal internal boundary layers during onshore flows. Boundary-Layer Meteorol 16(4):487–514

    Article  Google Scholar 

  • Rodean HC (1996) Stochastic Lagrangian models of turbulent diffusion. Springer, New York

    Book  Google Scholar 

  • Schmidt H, Schumann U (1989) Coherent structure of the convective boundary layer derived from large-eddy simulations. J Fluid Mech 200:511–562

    Article  Google Scholar 

  • Shao Y (1992) Turbulent dispersion in coastal atmospheric boundary layers: an application of a lagrangian model. Boundary-Layer Meteorol 59(4):363–385

    Article  Google Scholar 

  • Shao Y, Hacker JM (1990) Local similarity relationships in a horizontally inhomogeneous boundary layer. Boundary-Layer Meteorol 52(1–2):17–40

    Article  Google Scholar 

  • Shao Y, Hacker JM, Schwerdtfeger P (1991) The structure of turbulence in a coastal atmospheric boundary layer. Q J R Meteorol Soc 117(502):1299–1324

    Article  Google Scholar 

  • Smedman AS, Hoegstroem U (1983) Turbulent characteristics of a shallow convective internal boundary layer. Boundary-Layer Meteorol 25(3):271–287

    Article  Google Scholar 

  • Sorbjan Z (1989) Structure of the atmospheric boundary layer. Prentice-Hall, New Jersey

    Google Scholar 

  • Sorbjan Z (1990) Similarity scales and universal profiles of statistical moments in the convective boundary layer. J Appl Meteorol Climatol 29(8):762–775

    Article  Google Scholar 

  • Sorbjan Z (1991) Evaluation of local similarity functions in the convective boundary layer. J Appl Meteorol Climatol 30(12):1565–1583

    Article  Google Scholar 

  • Sorbjan Z (2007) A numerical study of daily transitions in the convective boundary layer. Bound-Layer Meteorol 123(3):365–383

  • Sreenivasan KR (1995) On the universality of the Kolmogorov constant. Phys Fluids 7(11):2778–2784

    Article  Google Scholar 

  • Stunder M, Sethuraman S (1985) A comparative evaluation of the coastal internal boundary-layer height equations. Boundary-Layer Meteorol 32(2):177–204

    Article  Google Scholar 

  • Tennekes H (1973) A model for the dynamics of the inversion above a convective boundary layer. J Atmos Sci 30(4):558–567

    Article  Google Scholar 

  • Tennekes H (1982) Similarity relations, scaling laws and spectral dynamics. In: Dop HV (ed) Nieuwstadt FTM. Atmospheric turbulence and air pollution modelling. Reidel, Kufstein, pp 37–68

    Google Scholar 

  • Thomson D (1987) Criteria for the selection of stochastic models of particle trajectories in turbulent flows. J Fluid Mech 180:529–556

    Article  Google Scholar 

  • Venkatram A (1977) A model of internal boundary-layer development. Boundary-Layer Meteorol 11(4):419–437

    Article  Google Scholar 

  • Vetterling WT, Press WH, Teukolsky SA, Flannery BP (2002) Numerical recipes example book (C++): the art of scientific computing. Cambridge University Press, Cambridge

    Google Scholar 

  • Wei J, Tang G, Zhu X, Wang L, Liu Z, Cheng M, Münkel C, Li X, Wang Y (2018) Thermal internal boundary layer and its effects on air pollutants during summer in a coastal city in north China. J Environ Sci 70:37–44

    Article  Google Scholar 

  • Weil J (1989) Stochastic modeling of dispersion in the convective boundary layer. In: van Dop H (ed) Air pollution modeling and its application VII. Springer, Boston, pp 437–449

    Chapter  Google Scholar 

  • Weil J (1990) A diagnosis of the asymmetry in top-down and bottom-up diffusion using a Lagrangian stochastic model. J Atmos Sci 47(4):501–515

    Article  Google Scholar 

  • Weil JC, Snyder WH, Lawson RE, Shipman MS (2002) Experiments on buoyant plume dispersion in a laboratory convection tank. Boundary-Layer Meteorol 102(3):367–414

    Article  Google Scholar 

  • Weil JC, Sullivan PP, Patton EG, Moeng CH (2012) Statistical variability of dispersion in the convective boundary layer: ensembles of simulations and observations. Boundary-Layer Meteorol 145(1):185–210

    Article  Google Scholar 

  • Weisman B (1976) On the criteria for the occurrence of fumigation inland from a large lake. Atmos Environ 10:172–173

    Article  Google Scholar 

  • Wilczak JM, Oncley SP, Stage SA (2001) Sonic anemometer tilt correction algorithms. Boundary-Layer Meteorol 99(1):127–150

    Article  Google Scholar 

  • Wyngaard JC (1985) Structure of the planetary boundary layer and implications for its modeling. J Appl Meteorol Climatol 24(11):1131–1142

    Article  Google Scholar 

  • Wyngaard JC (1988) Structure of the PBL. In: Wyngaard JC, Venkatram A (eds) Air pollution modeling. American Meteorological Society, Massachusetts, pp 9–57

    Chapter  Google Scholar 

  • Wyngaard JC, Brost RA (1984) Top-down and bottom-up diffusion of a scalar in the convective boundary layer. J Atmos Sci 41(1):102–112

    Article  Google Scholar 

Download references

Acknowledgements

This study has been developed within the context of a Research & Development project regulated by the Brazilian National Agency for Electric Energy and sponsored by the companies Linhares Geração S.A. and Termelétrica Viana S.A. The authors are grateful for the support provided by these companies for the development of the present work. The authors also thank the Brazilian agencies CAPES (Coordenação de Aperfeiçoamento de Pessoal de Ensino Superior) and CNPq (Conselho Nacional de Desenvolvimento Científico e Tecnológico) for financial support of the research.

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Appendices

Appendix 1: Uncertainty on the Linear Fit

The linear adjustment performance is evaluated using two goodness-of-fit measures: R-squared (\(R^2\)) and the standard error of the regression (S) defined respectively as

$$\begin{aligned} S = \sqrt{\frac{1}{(N-2)}\sum _{i=1}^{N}\left( y_i-\hat{y_i}\right) ^2} \end{aligned}$$
(30)

and

$$\begin{aligned} R^2=1-\frac{\sum _{i=1}^{N}\left( y_i-\hat{y_i} \right) ^2}{\sum _{i=1}^{N}\left( y_i-\overline{y} \right) ^2}, \end{aligned}$$
(31)

where y are the original measurements, \(\hat{y}\) are the estimated values of y, and N is the total number of measurements.

The percentage relative uncertainty of the linear (\(dA=100\sigma _A/A\)) and angular (\(dB=100\sigma _B/B\)) estimated coefficients using the linear fit method have been evaluated as (Bevington and Robinson 2003)

$$\begin{aligned} \sigma _A=S\sqrt{\left( \frac{\sum _{i=1}^Nx_i^2}{\varDelta }\right) } \end{aligned}$$
(32)

and

$$\begin{aligned} \sigma _B=S\sqrt{\frac{N}{\varDelta }}, \end{aligned}$$
(33)

where

$$\begin{aligned} \varDelta =N\sum _{i=1}^Nx_i^2-\left( \sum _{i=1}^Nx_i\right) ^2. \end{aligned}$$
(34)

The absolute and percentage relative uncertainty on \(z_i\) due the linear fit is obtained, respectively, as

$$\begin{aligned} \sigma _{z_i}=\sqrt{\left( \frac{\partial z_i}{\partial A} \right) ^2\sigma _A^2 + \left( \frac{\partial z_i}{\partial B} \right) ^2\sigma _B^2} \end{aligned}$$
(35)

and

$$\begin{aligned} dz_i=100\frac{\sigma _{z_i}}{z_i}. \end{aligned}$$
(36)

Appendix 2: Uncertainty on the Adjusted Turbulence Parameters Profiles

Vertical profiles of the turbulence parameters are used to adjust analytical relationships found in the literature. To reduce the uncertainty in the adjusted parameters due the outliers, we present the following methodology: a first adjustment is obtained by the nonlinear least-squares method; assuming that the error between experimental data and the modelled curve is normally distributed, error values larger than three standard errors with respect to the mean are marked as outliers; a second fit is performed using the retained measurements.

The uncertainty on the adjusted parameter can be obtained directly from the covariance matrix \(\mathbf{C} = \mathbf{A} ^{-1}\) as (Vetterling et al. 2002)

$$\begin{aligned} \sigma _{\alpha _j}=\sqrt{C_{jj}}, \end{aligned}$$
(37)

where

$$\begin{aligned} A_{jk} =\sum _i\frac{1}{\sigma _i^2}\left( \frac{\partial f(x_i;\alpha _0...\alpha _{m-1})}{\partial \alpha _j} \right) \left( \frac{\partial f(x_i;\alpha _0...\alpha _{m-1})}{\partial \alpha _k} \right) \end{aligned}$$
(38)

are the elements of the matrix A\(_{M\times M}\), and where m is the number of unknown parameters. In Eq. 38, \(x_i\) are the measured dependent variables, \(\sigma _i\) is the measurement error of the ith data point, \(\alpha _j=\alpha _0...\alpha _{m-1}\) are the parameters to be evaluated, and f is the model function.

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Martins, L.G.N., Acevedo, O.C., Puhales, F.S. et al. Vertical Profiles of Turbulence Parameters in the Thermal Internal Boundary Layer. Boundary-Layer Meteorol 179, 423–446 (2021). https://doi.org/10.1007/s10546-020-00603-z

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