Uncertainties in measurement and modelling of net ecosystem exchange of a forest

被引:43
作者
Rannik, Ullar
Kolari, Pasi
Vesala, Timo
Hari, Pertti
机构
[1] Univ Helsinki, Dept Phys Sci, FIN-00014 Helsinki, Finland
[2] Univ Helsinki, Dept Forest Ecol, FIN-00014 Helsinki, Finland
基金
芬兰科学院;
关键词
net ecosystem exchange; eddy covariance; optimal model; forest ecosystem; systematic and random errors;
D O I
10.1016/j.agrformet.2006.05.007
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
At Hyyiala, SMEAR II measurement station in Southern Finland, the eddy covariance (EC) measurements of ecosystem exchange were performed above a Scots pine forest with two closely positioned flux measurement systems. The separation distance of about 30 m between the two systems surrounded by a homogeneous stand of the radius 200 m implies practically the same micrometeorological flux measurement source area, but partial decorrelation and different observation of turbulence and fluxes due to spatial separation. Thus, these fluxes provide two not fully independent estimates of net ecosystem exchange (NEE) of the same forest. NEE, obtained from the EC measurements, was intercompared. with modelled values for periods consisting of several months of observations. The measurements as well as model values were studied for random errors as well as systematic differences. The process-based canopy exchange model was as successful as direct EC measurements in estimation of NEE in terms of random errors and systematic biases in NEE and serves as a useful tool for studying the canopy processes and gap-filling of missing values in measurements. As the EC technique is not free of possible error sources, modelling is also useful for evaluation of flux measurements. The important conclusion of current study is that the main uncertainty of long-term ecosystem NEE does not possibly result from underestimation of night-time observations as commonly believed, but could be instead related to day-time observations. For the given site, the yearly uncertainty of annual NEE was estimated to be 80 gC m(-2) year(-1), originating mainly from the uncertainty of day-time observations. (c) 2006 Elsevier B.V. All rights reserved.
引用
收藏
页码:244 / 257
页数:14
相关论文
共 39 条
[1]  
Aalto Tuula, 1998, Silva Fennica, V32, P321
[2]  
Aubinet M, 2000, ADV ECOL RES, V30, P113, DOI 10.1016/S0065-2504(08)60018-5
[3]  
Baldocchi D, 2001, B AM METEOROL SOC, V82, P2415, DOI 10.1175/1520-0477(2001)082<2415:FANTTS>2.3.CO
[4]  
2
[5]   Assessing the eddy covariance technique for evaluating carbon dioxide exchange rates of ecosystems: past, present and future [J].
Baldocchi, DD .
GLOBAL CHANGE BIOLOGY, 2003, 9 (04) :479-492
[6]  
Cowan I. R., 1977, Advances in Botanical Research, V4, P117, DOI 10.1016/S0065-2296(08)60370-5
[7]   Turbulence in plant canopies [J].
Finnigan, J .
ANNUAL REVIEW OF FLUID MECHANICS, 2000, 32 :519-571
[8]   A re-evaluation of long-term flux measurement techniques - Part I: Averaging and coordinate rotation [J].
Finnigan, JJ ;
Clement, R ;
Malhi, Y ;
Leuning, R ;
Cleugh, HA .
BOUNDARY-LAYER METEOROLOGY, 2003, 107 (01) :1-48
[9]   Sonic anemometer (co)sine response and flux measurement I. The potential for (co)sine error to affect sonic anemometer-based flux measurements [J].
Gash, JHC ;
Dolman, AJ .
AGRICULTURAL AND FOREST METEOROLOGY, 2003, 119 (3-4) :195-207
[10]   Annual pattern of photosynthesis in Scots pine in the boreal zone [J].
Hari, P ;
Mäkelä, A .
TREE PHYSIOLOGY, 2003, 23 (03) :145-155