A Re-Evaluation of Long-Term Flux Measurement Techniques Part I: Averaging and Coordinate Rotation

By J. Finnigan, R. Clement, Yadvinder S. Malhi, R. Leuning, H. Cleugh. 2003

638 citations recorded by the source corpus.

Subfields: Atmospheric Science, Computational Mechanics, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/6c3798ffc1a544e7ccabe0c0c0bfadf2419c4596

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Citations in the corpus

The Influence of Idealized Heterogeneity on Wet and Dry Planetary Boundary Layers Coupled to the Land Surface. (2005, background): “The practice of forcing average vertical velocity to zero becomes especially uncertain in the presence of surface heterogeneity (e.g., Finnigan et al. 2003).”
The productivity, metabolism and carbon cycle of tropical forest vegetation (2012, neutral): “Such attempts at quantifyingNEEhave generally proved frustrating in the tropical forest environment, where there is a tendency for night-time respiration to be underestimated as cool, carbon dioxide-rich air tends to pool and flow laterally in the belowcanopy air space (Finnigan et al. 2003; Araujo ”
The energy balance closure problem: an overview. (2008, methodology): “Furthermore, in recent papers it was found that time-averaged fluxes (Finnigan et al. 2003) or spatially averaged fluxes including turbulent organized structures (Kanda et al. 2004) can close the energy balance.”
Annual carbon balance of a managed wetland meadow in the Somerset Levels, UK (2006, neutral): “, 2004) and possible shortcomings in the eddy correlation methodology itself (Finnegan et al., 2003), together with an error discovered by Li-Cor in the electronic response time of the Li-7500 which affected the lag time between the Solent and the Li-7500.”
Effects of different eddy covariance correction schemes on energy balance closure and comparisons with the modified Bowen ratio system (2008, background): “…that the choice of averaging period is an additional facet of the EC processing that can have a substantial effect on the observed energy balance (Finnigan et al., 2003; Cava et al., 2007), because short averaging intervals act as a high pass filter that can remove low-frequency components of…”
A simple unified theory for flow in the canopy and roughness sublayer (2007, background): “In these circumstances it is expected that a drainage current forms within the canopy due to the slight slope at the site ( Finnigan et al. 2003; Leuning et al. 2005).”