A 2-DIMENSIONAL TRAJECTORY-SIMULATION MODEL FOR NON-GAUSSIAN, INHOMOGENEOUS TURBULENCE WITHIN PLANT CANOPIES

被引:110
作者
FLESCH, TK
WILSON, JD
机构
[1] Division of Meteorology, Department of Geography, University of Alberta, Edmonton, T6G 2H4, Alberta
关键词
D O I
10.1007/BF00119097
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
We report a two-dimensional (alongwind u, vertical w) trajectory-simulation model, consistent with Thomson's (1987) well-mixed criteria, that allows for the non-Gaussian turbulence typical of flow within a plant canopy. The effect of non-Gaussian turbulence was examined by formulating a non-Gaussian u, w joint probability density function (PDF) as the sum of two Gaussian joint-PDFs. The resultant PDF reproduced the desired means, variances, skewnesses, and kurtoses, and the correct covariance. In prediction of the location of maximum concentration downwind of a line source in homogeneous, slightly non-Gaussian turbulence, it proved advantageous to incorporate skewness and kurtosis. However, in the case of inhomogeneous. highly non-Gaussian turbulence, the addition of skewness and kurtosis in the model resulted in substantially worse agreement with measurements than the results of the model using Gaussian PDFs. This may be due to inaccuracy in our PDF formulation. Dispersion predictions from the model with Gaussian PDFs were generally not statistically different from measurements. These results indicate that a two-dimensional Gaussian trajectory-simulation approach is adequate to predict mean concentrations and fluxes resulting from sources within plant canopies.
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页码:349 / 374
页数:26
相关论文
共 33 条
[1]   COMPARISON OF TURBULENCE STATISTICS WITHIN 3 BOREAL FOREST CANOPIES [J].
AMIRO, BD .
BOUNDARY-LAYER METEOROLOGY, 1990, 51 (1-2) :99-121
[2]  
BAERENTSEN JH, 1984, ATMOS ENVIRON, V18, P701, DOI 10.1016/0004-6981(84)90256-7
[3]   THE EFFECTS OF EXTREME TURBULENT EVENTS ON THE ESTIMATION OF AERODYNAMIC VARIABLES IN A DECIDUOUS FOREST CANOPY [J].
BALDOCCHI, DD ;
MEYERS, TP .
AGRICULTURAL AND FOREST METEOROLOGY, 1989, 48 (1-2) :117-134
[4]   EXPERIMENTS ON SCALAR DISPERSION WITHIN A MODEL-PLANT CANOPY .2. AN ELEVATED PLANE SOURCE [J].
COPPIN, PA ;
RAUPACH, MR ;
LEGG, BJ .
BOUNDARY-LAYER METEOROLOGY, 1986, 35 (1-2) :167-191
[5]   AN APPLICATION OF THE LANGEVIN EQUATION FOR INHOMOGENEOUS CONDITIONS TO DISPERSION IN A CONVECTIVE BOUNDARY-LAYER [J].
DEBAAS, AF ;
VANDOP, H ;
NIEUWSTADT, FTM .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1986, 112 (471) :165-180
[6]  
DURBIN PA, 1981, BOUND-LAY METEOROL, V29, P409
[7]  
DURBINPA, 1983, NASA REFERENCE PUBLI, V1103
[8]  
Gardiner C.W, 1983, HDB STOCHASTIC METHO
[9]  
HALL CD, 1975, Q J ROY METEOR SOC, V101, P235, DOI 10.1002/qj.49710142807
[10]  
HANNA SR, 1978, 4TH P AMS S TURB DIF, P14