Abstract
Little is known about in-canopy processes that may alter forest–atmosphere exchanges of trace gases and aerosols. To improve our understanding of in-canopy mixing, we use large-eddy simulation to study the effect of scalar source/sink distributions on scalar concentration moments, fluxes, and correlation coefficients within and above an ideal forest canopy. Scalars are emitted from: (1) the ground, (2) the canopy, and (3) both the ground and the canopy; a scalar is also deposited onto the canopy. All scalar concentration moments, fluxes, and correlation coefficients are affected by the source location/distribution, as is the scalar segregation intensity. We conclude that vertical source/sink distribution has a profound impact on scalar concentration profiles, fluxes, correlation coefficient, and scalar segregation.
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References
Auger L, Legras B (2007) Chemical segregation by heterogeneous emissions. Atmos Environ 41: 2303–2318
Baldocchi DD, Meyers TP (1991) Trace gas-exchange above the floor of a a deciduous forest 1. Evaporation and CO2 efflux. J Geophys Res-Atmos 96: 7271–7285
Baldocchi DD, Guenther A, Harley P et al (1995) The fluxes and air chemistry of isoprene above a deciduous hardwood forest. Philos Trans Roy Soc A 351: 279–296
Bohm M, Raupach MR, Finnigan JJ (2000) The effect of scalar source distribution on eddy diffusivities and bulk transfer coefficients. In: Proceedings of 24th conference on Agricultural and forest meteorology, Davis, CA, USA
Brown KW, Covey W (1966) The energy budget evaluation of the micrometeorology logical transfer processes within a cornfield. Agric For Meteorol 3: 73–96
Cassini M, Radicchi A, Albertson JD (2007) Modelling of concentration fluctuations in canopy turbulence. Boundary-Layer Meteorol 122: 655–681
Coppin PA, Raupach MR, Legg BJ (1986) Experiments on scalar dispersion within and model plant canopy 2: An elevated plane source. Boundary-Layer Meteorol 35: 167–191
Deardorff JW (1980) Stratocumulus-capped mixed layers derived from a three-dimensional model. Boundary-Layer Meteorol 18: 495–527
de Arellano JVG (2003) Bridging the gap between atmospheric physics and chemistry in studies of small scale turbulence. Bull Am Meteorol Soc 84: 51–56
Denmead OT, Bradley EF (1987) On scalar transport in plant canopies. Irrig Sci 8: 131–149
Finnigan JJ (2000) Turbulence in plant canopies. Annu Rev Fluid Mech 32: 519–571
Finnigan JJ, Shaw RH (2008) Double-averaging methodology and its application to turbulent flow in and above vegetation canopies. Acta Geophys 56: 534–561
Finnigan JJ, Shaw RH, Patton EG (2009) Turbulence structure above a vegetation canopy. J Fluid Mech 637: 387–424
Fuentes JD, Wang D, Bowling DR et al (2007) Biogenic hydrocarbon chemistry within and above a mixed deciduous forest. J Atmos Chem 56: 165–185
Gao W, Shaw R, Paw UKT (1989) Observation of organized structure in turbulent-flow within and above a forest canopy. Boundary-layer Meteorol 47: 349–377
Guenther A, Baugh W, Davis K et al (1996) Isoprene fluxes measured by enclosure, relaxed eddy accumulation, surface layer gradient, mixed layer gradient, and mixed layer mass balance techniques. J Geophys Res-Atmos 101: 18555–18567
Guenther A, Karl T, Harley P et al (2006) Estimates of global terrestrial isoprene emissions using MEGAN (Model of Emissions of Gases and Aerosols from Nature). Atmos Chem Phys 6: 3181–3210
Haugen DA, Kaimal JC, Bradley EF (1971) An experimental study of Reynolds stress and heat flux in the atmospheric boundary layer. Q J R Meteorol Soc 97: 349–377
Jardine K, Harley P, Karl T et al (2008) Plant physiological and environmental controls over the exchange of acetaldehyde between forest canopies and the atmosphere. Biogeosciences 5: 1559–1572
Karl T, Harley P, Guenther A et al (2005) The bi-directional exchange of oxygenated VOCs between a loblolly pine (Pinus taeda) plantation and the atmosphere. Atmos Chem Phys 5: 3015–3031
Krol MC, Molemaker J, de Arellano JVG (2000) Effects of turbulence and heterogeneous emissions on the active species in the convective boundary layer. J Geophys Res 105: 6871–6884
Lee XH, Black TA (1993) Atmospheric turbulence within and above a Douglas-Fir Stand 2. Eddy Fluxes of sensible heat and water vapor. Boundary-Layer Meteorol 64: 369–389
Moeng CH (1984) A large eddy simulation model for the study of planetary boundary-layer turbulence. J Atmos Sci 41: 2052–2062
Moeng C, Sullivan P (1994) A comparison of shear-driven and buoyancy-driven planetary boundary layers. J Atmos Sci 51: 999–1022
Moeng C, Wyngaard J (1988) Spectral analysis of large eddy simulations of the convective boundary layer. J Atmos Sci 45: 3573–3587
Patton EG, Davis KJ, Barth MC, Sullivan PP (2001) Decaying scalars emitted by a forest canopy: a numerical study. Boundary-Layer Meteorol 100: 91–129
Patton E, Sullivan P, Davis K (2003) The influence of a forest canopy on top-down and bottom-up diffusion in the planetary boundary layer. Q J R Meteorol Soc 129: 1415–1434
Patton E, Sullivan P, Moeng C (2005) The influence of idealized heterogeneity on wet and dry planetary boundary layers coupled to the land surface. J Atmos Sci 65: 2078–2097
Pope S (2000) Turbulent flows. Cambridge University Press, Cambridge 771 pp
Rannik U, Keronen P, Hari P, Vesala T (2004) Estimation of forest–atmosphere CO2 exchange by eddy covariance and profile techniques. Agric For Meteorol 126: 141–155
Raupach MR, Shaw RH (1982) Averaging procedures for flow within vegetation canopies. Boundary-Layer Meteorol 22: 79–90
Raupach MR, Finnigan JJ, Brunet Y (1996) Coherent eddies and turbulence in vegetation canopies: the mixing layer analogy. Boundary-Layer Meteorol 78: 351–382
Schmid HP, Su HB, Vogel CS, Curtis, PS (2003) Ecosystem–atmosphere exchange of carbon dioxide over a mixed hardwood forest in northern lower Michigan. J Geophys Res-Atmos. doi:10.1029/2002JD003011
Shaw RH, Schumann U (1992) Large eddy simulation of turbulent flow above and within a forest. Boundary-Layer Meteorol 61: 47–64
Shen S, Leclerc M (1997) Modelling the turbulence structure in the canopy layer. Agric For Meteorol 87: 3–25
Spalart P, Moser R, Rogers M (1991) Spectral methods for the Navier–Stokes equations with one infinite and two periodic directions. J Comput Phys 96: 297–324
Sparks JP, Monson R, Sparks K, Lerdau M (2001) Leaf uptake of nitrogen dioxide (NO2) in a tropical wet forest: implications for tropospheric chemistry. Oecologia 127: 214–221
Su HB, Shaw R, Paw UK, Moeng C, Sullivan P (1998) Turbulence statistics of neutrally stratified flow within and above a sparse forest from large eddy simulations and field observations. Boundary-Layer Meteorol 88: 363–397
Sullivan PP, Patton EG (2008) A highly parallel algorithm for turbulence simulations in planetary boundary layers: Results with meshes up to 10243. In: Proceedings of 18th American Meteorological Society, Stockholm, Sweden, June 2008
Sullivan PP, Patton EG (2011) The effect of mesh resolution on convective boundary layer statistics and structures generated by large-eddy simulation. J Atmos Sci 68: 2395–2415
Thom AS (1971) Momentum absorption by vegetation. Q J R Meteorol Soc 97: 414–428
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Edburg, S.L., Stock, D., Lamb, B.K. et al. The Effect of the Vertical Source Distribution on Scalar Statistics within and above a Forest Canopy. Boundary-Layer Meteorol 142, 365–382 (2012). https://doi.org/10.1007/s10546-011-9686-1
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DOI: https://doi.org/10.1007/s10546-011-9686-1