Turbulence statistics inside and over forest:: Influence on footprint prediction

被引:80
作者
Rannik, Ü [1 ]
Markkanen, T
Raittila, J
Hari, P
Vesala, T
机构
[1] Univ Helsinki, Dept Phys Sci, Helsinki, Finland
[2] Univ Helsinki, Dept Forest Ecol, Helsinki, Finland
关键词
flux footprints; forest canopy; Lagrangian trajectory simulation; turbulence statistics; LAGRANGIAN STOCHASTIC-MODELS; ATMOSPHERIC SURFACE-LAYER; PLANT CANOPIES; ARBITRARY STRUCTURE; FIELD-MEASUREMENTS; DECIDUOUS FOREST; REYNOLDS STRESS; FLUXES; TRAJECTORIES; DISPERSION;
D O I
10.1023/A:1025404923169
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Observations of wind statistics within and above a Scots pine forest are compared with those predicted from an analytical second-order closure model. The roughness sublayer (RSL) effects, and the influence of stability on similarity functions, are studied using observations. The commonly accepted forms of similarity functions describe the influence of diabatic effects above the RSL well. According to earlier studies they are expected also to apply within the RSL. As an exception, the average wind speed normalised with friction velocity was found to be invariant with stability close to the canopy top under unstable conditions. Lagrangian stochastic trajectory simulations were used to evaluate the influence of canopy turbulence profiles on footprint prediction. The main uncertainty was found to arise from parameterisation of the random forcing term in the Lagrangian velocity equation. The influence of diabatic conditions was studied, and it was found that thermal stability affects significantly the footprint function above the forest canopy, but significant uncertainty exists because of uncertainties in the formulation of stability functions.
引用
收藏
页码:163 / 189
页数:27
相关论文
共 49 条
[1]   Estimation of the Lagrangian structure function constant C0 from surface-layer wind data [J].
Anfossi, D ;
Degrazia, G ;
Ferrero, E ;
Gryning, SE ;
Morselli, MG ;
Castelli, ST .
BOUNDARY-LAYER METEOROLOGY, 2000, 95 (02) :249-270
[2]  
Aubinet M, 2000, ADV ECOL RES, V30, P113, DOI 10.1016/S0065-2504(08)60018-5
[3]   Flux footprints within and over forest canopies [J].
Baldocchi, D .
BOUNDARY-LAYER METEOROLOGY, 1997, 85 (02) :273-292
[4]   FLUX GRADIENT RELATIONSHIPS ABOVE TALL PLANT CANOPIES [J].
CELLIER, P ;
BRUNET, Y .
AGRICULTURAL AND FOREST METEOROLOGY, 1992, 58 (1-2) :93-117
[5]   DEFINING LEAF-AREA INDEX FOR NON-FLAT LEAVES [J].
CHEN, JM ;
BLACK, TA .
PLANT CELL AND ENVIRONMENT, 1992, 15 (04) :421-429
[6]  
Fazu C, 1989, Q J ROY METEOR SOC, V115, P335, DOI [10.1002/qj.49711548607, DOI 10.1002/QJ.49711548607]
[7]   Turbulence in plant canopies [J].
Finnigan, J .
ANNUAL REVIEW OF FLUID MECHANICS, 2000, 32 :519-571
[9]   FOOTPRINT ESTIMATION FOR SCALAR FLUX MEASUREMENTS IN THE ATMOSPHERIC SURFACE-LAYER [J].
HORST, TW ;
WEIL, JC .
BOUNDARY-LAYER METEOROLOGY, 1992, 59 (03) :279-296
[10]  
HORST TW, 1994, J ATMOS OCEAN TECH, V11, P1018, DOI 10.1175/1520-0426(1994)011<1018:HFIFET>2.0.CO