[1]Goulden M L, Munger J W, Fan S-M, et al. Measurements of carbon sequestration by long-term eddy covariance: Methods and a critical evaluation of accuracy[J]. Global Change Biology, 1996,2:169-182. [2]Baldocchi D D, Hicks B B, Meyers T P. Measuring biosphere-atmosphere exchange of biologically related gases with micrometeorological methods[J]. Ecology, 1988,69:1 331-1 340. [3]Wofsy S C, Goulden M L, Munger J W,et al. Net exchange of CO2 in a midlatitude forest[J]. Science,1993,260:1 314-1 317. [4]Berbigier P, Bonnefond J M, Mellmann P. CO2 and water vapor fluxes for 2 years above Euroflux forest site[J]. Agricultural and Forest Meteorology, 2001, 108: 183-197. [5]Grace J, Lloyd J, Mclntyre J, et al. Carbon dioxide uptake by an undisturbed tropical rain in southwest Amazonia,1992-1993[J]. Science,1995,270:778-780. [6]Black T A, den Hartog G, Neumann H H, et al. Annual cycles of water vapor and carbon dioxide fluxes in and above a boreal aspen forest[J]. Global Change Biology, 1996,2:219-229. [7]Goulden M L, Munger J W, Fan S-M, et al. Exchange of carbon dioxide by a deciduous forest: Response to interannual climate variability[J]. Science, 1996,271: 1 576-1 578. [8]Baldocchi D, Falge E, Gu L H, et al. Fluxnet: A new tool to study the temporal and spatial variability of ecosystem-scale carbon dioxide, water vapor, and energy flux densities[J].Bulletin of the American Meteorological Society, 2001,82: 2 415-2 434. [9]Lee X, Hu X Z. Forest-air fluxes of carbon, water and energy over non-flat terrain[J]. Boundary-Layer Meteorology, 2002,103:277-301. [10]Lee X.On micrometeorological observation of surface-air exchange over tall vegetation[J].Agricultural and Forest Meteorology, 1998,91:39-49. [11]Leuning R, King K M. Comparison of eddy-covariance measurement of CO2 fluxes by open- and closed-path CO2 analysers[J].Boundary-Layer Meteorology, 1992,59: 297-311. [12]Suyker A E, Verma S B. Eddy correlation measurement of CO2 flux using a closed-path sensor: Theory and field test against an open path sensor[J].Boundary-Layer Meteorology, 1993,64:391-407. [13]Paw U K T, Baldocchi D D, Meyers T P, et al. Correction of eddy-covariance measurements incorporating both advective effects and density fluxs[J].Boundary-Layer Meteorology, 2000,97:487-511. [14]Massman W J, Lee X. Eddy covariance flux corrections and uncertainties in long term studies of carbon and energy exchanges[J].Agricultural and Forest Meteorology, 2002, 113: 121-144. [15]Foken T , Wichra B. Tools for quality assessment of surface measurement[J].Agricultural and Forest Meteorology, 1995,78:83-105. [16]Moncrieff J B, Malhi Y, Leuning R. The propagation of errors in long-term measurement of land-atmosphere fluxes of carbon and water[J]. Global Change Biology,1996,2:231-240. [17]Businger J A. Evaluation of the accuracy with which dry deposition can be measured with current micrometeorological technique[J]. Journal of Climate and Applied Meteorology, 1986,25:1 100-1 124. [18]Webb E K, Pearman G I, Leuning R. Correction of flux measurement for density effects due to heat and water vapour transfer[J]. Quarterly Journal Royal Meteorological Society, 1980,106:85-100. [19]Baldcchi D,Finnigan J, Wilson K, et al. On measuring net carbon exchange over tall vegetation on complex terrain[J]. Boundary-Layer Meteorology, 2000,96:257-291. [20]Moore C J. Frequency reponse correction for eddy correction systems [J]. Boundary-Layer Meteorology, 1986,37:17-30. [21]Horst T W. A simple formula for attenuation of eddy fluxes measured with firstorderresponse scalar sensors[J]. Boundary-Layer Meteorology, 1997,82:219-233. [22]Massman W J. A simple method for estimating frequency response correction for eddy covariance systems[J]. Agricultural Forest and Meteorology, 2000,104:185-198. [23]Massman W J. Reply to comment by Rannik on “A simple method for estimating frequency response correction for eddy covariance systems”[J]. Agricultural Forest and Meteorology,2001,107:247-251. [24]Rannik U. A comment on the paper by W.J.Masman “A simple method for estimating frequency response correction for eddy covariance systems”[J]. Agricultural Forest and Meteorology,2001,107:241-245. [25]Goulden M L, Daube B C, Fan SM, et al. Physiological reponse of a black spruce forest to the weather[J]. Journal of Geophysical Research, 1997,102:28 987-28 996. [26]Finnigan J. A commnent on the paper by Lee(1998): “On micrometeorological observation of surface-air exchange over tall vegetation”[J]. Agricultural Forest and Meteorology, 1999,97:55-64. [27]Kaimal J C, Finnigan J J. Atmospheric Boundary Layer Flows-Their Structure and Measurement[M]. New York: Oxford University Press, 1994. [28]Wilczak J M, Oncley S P, Stage S A. Sonic anemometer tilt correction algorithms[J]. Boundary-Layer Meteorology, 2001,99:127-150. [29]Weber R O. Remarks on the definition and estimation of friction velocity[J]. Boundary-Layer Meteorology,1999,93:107-209. [30]Lecler M Y, Thertell G W. Footprint prediction of scalar using a markovian analysis[J]. Boundary-Layer Meteorology, 1990,52:247-258. [31]Schmid H P. Source areas for scalar and scalar flues[J]. Boundary-Layer Meteorology, 1994,67:293-318. [32]Lee X, Barr A G. Climatology of gravity waves in a forest[J]. Quarterly Journal Royal Meteorological Society, 1998,124:1 403-1 419. [33]Fitzjarrald D R, Morre K E. Mechanisms of nocturnal exchange between the rain forest and the atmosphere[J]. Journal of Geophysical Research, 1990,95:16 938-16 850. [34]Hu X, Lee X, Steven D E, et al. A numerical study of noctural wavelike motion in forest[J]. Boundary-Layer Meteorology, 2002,102:199-223. [35]Wyngaard J, Kosovic B. Similarity of structurefuction parameters in the stratified boundarylayer[J]. Boundary-Layer Meteorology, 1994,71:277-296. [36]Mahrt L. Momentum balance of gravity flow[J]. Journal of the Atmospheric Sciences, 1982,39:2 701-2 711. [37]Sun J, Desjardins R, Mahrt L, et al. Transport of carbon dioxide, water vapour, and ozone by turbulence and local circulations[J].Journal of Geophysical Reaearch, 1998, 103:25 873-25 885. [38]Black T A, Chen W J, Barr A G, et al. Increased carbon sequestration by s boreal deciduous forest in years with a warm spring[J]. Geophysical Research Letters, 2000,27: 1 271-1 274. [39]Aubinet M, Grelle A, Ibrom A, et al. Estimates of the annual net carbon and water exchange of forest: The EUROFLUX methodology[J]. Advances in Ecological Research, 2000,30:113-175. [40]Grace J, Malhi Y, Lloyd J, et al.The use of eddy covariance to infer the carbon dioxide uptake of Brazilian rain forest[J]. Global Change Biology, 1996,2:209-217. |