2001
DOI: 10.1016/s0168-1923(01)00244-1
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Long term carbon dioxide exchange above a mixed forest in the Belgian Ardennes

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Cited by 372 publications
(225 citation statements)
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“…Many studies continue to use the rectangular hyperbola (Wofsy et al, 1993;Aubinet et al, 2001;Pilegaard et al, 2001) including those focusing on remote sensing (Ruimy et al, 1995;Xiao, 2006). By using 10-day periods for parameter estimation, one loses the hysteresis effect and can mask the curvature of the diurnal light response (Biscoe et al, 1975;Ham et al, 1995;Gilmanov et al, 2003) but, again, if using the results presented here in continental scale models, only a restricted amount of information can be incorporated and as few parameters as possible is desirable.…”
Section: Discussionmentioning
confidence: 99%
“…Many studies continue to use the rectangular hyperbola (Wofsy et al, 1993;Aubinet et al, 2001;Pilegaard et al, 2001) including those focusing on remote sensing (Ruimy et al, 1995;Xiao, 2006). By using 10-day periods for parameter estimation, one loses the hysteresis effect and can mask the curvature of the diurnal light response (Biscoe et al, 1975;Ham et al, 1995;Gilmanov et al, 2003) but, again, if using the results presented here in continental scale models, only a restricted amount of information can be incorporated and as few parameters as possible is desirable.…”
Section: Discussionmentioning
confidence: 99%
“…Of course, these soil respiration values cannot be directly compared to those of the ER obtained using an eddy-covariance system for similar sites because the latter includes the aerial vegetation respiration. However, as the soil respiration is generally the major component of ER (Aubinet et al 2001;Davidson et al 2006b), it appears relevant that a high soil respiration leads also to a high ER measured by an eddy-covariance technique and therefore a higher ER d found for the two investigated sites, especially during the wet season (Figs. 8e and 9b-e).…”
Section: Larger Ecosystem Respiration (Er) For the Forest Than Savannahmentioning
confidence: 96%
“…(1) below as the algebraic sum of the turbulent flux (F CO2 ) measured by the eddy-covariance system and the CO 2 storage flux change in the air below the measurement point, considering the additional terms negligible (Aubinet et al 2001). The storage flux was computed using a single measurement point of the CO 2 concentration at a height of 18 m (forest) and 4.95 m (savannah) as applied in several studies in the Africa region by several authors (Archibald et al 2009;Merbold et al 2009;Ago et al 2014Ago et al , 2015.…”
Section: Data Treatment Analysis and Uncertainty Evaluationmentioning
confidence: 99%
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