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  Direct advection measurements do not help to solve the night-time CO2 closure problem: Evidence from three different forests

Aubinet, M., Feigenwinter, C., Heinesch, B., Bernhöfer, C., Canepa, E., Lindroth, A., et al. (2010). Direct advection measurements do not help to solve the night-time CO2 closure problem: Evidence from three different forests. Agricultural and Forest Meteorology, 150(5), 655-664. doi:10.1016/j.agrformet.2010.01.016.

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Aubinet, M., Author
Feigenwinter, C., Author
Heinesch, B., Author
Bernhöfer, C., Author
Canepa, E., Author
Lindroth, A., Author
Montagnani, L., Author
Rebmann, C.1, Author           
Sedlak, P., Author
Van Gorsel, E., Author
Affiliations:
1Department Biogeochemical Processes, Prof. E.-D. Schulze, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1497751              

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Free keywords: Advection Forests CO2 fluxes Eddy covariance net ecosystem exchange term eddy-covariance surface-air exchange long-term tall vegetation complex terrain micrometeorological observations alpine forest carbon fluxes
 Abstract: The ADVEX project involved conducting extensive advection measurements at three sites, each with a different topography. One goal of the project was to measure the [CO2] balance under night-time conditions, in an attempt to improve NEE estimates. Four towers were arranged in a square around a main tower, with the sides of the square about 100 m long. Equipped with 16 sonic anemometers and [CO2] sampling points, the towers were installed to measure vertical and horizontal advection of [CO2]. Vertical turbulent fluxes were measured by an eddy covariance system at the top of the main tower. The results showed that horizontal advection varied greatly from site to site and from one wind sector to another, the highest values being reached when there were large friction velocities and fairly unstable conditions. There was less variation in vertical advection, the highest values being reached when there were low friction velocities and stable conditions. The night-time NEE estimates deduced from the mass balance were found to be incompatible with biologically driven fluxes because (i) they varied strongly from one wind sector to another and this variation could not be explained in terms of a response of the biologic flux to climate, (ii) their order of magnitude was not realistic and (iii) they still showed a trend vs. friction velocity. From a critical analysis of the measurement and data treatment we concluded that the causes of the problem are related to the representativeness of the measurement (control volume size, sampling resolution) or the hypotheses underlying the derivation of the [CO2] mass balance (ignoring the horizontal turbulent flux divergence). This suggests that the improvement of eddy flux measurements by developing an advection completed [CO2] mass balance at night would be practically difficult. (C) 2010 Elsevier B.V. All rights reserved.

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Language(s): eng - English
 Dates: 2010
 Publication Status: Issued
 Pages: -
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 Rev. Type: -
 Identifiers: DOI: 10.1016/j.agrformet.2010.01.016
ISI: ://000278244400002
Other: BGC1350
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Title: Agricultural and Forest Meteorology
Source Genre: Journal
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Publ. Info: Amsterdam : Elsevier
Pages: - Volume / Issue: 150 (5) Sequence Number: - Start / End Page: 655 - 664 Identifier: CoNE: https://pure.mpg.de/cone/journals/resource/954928468040
ISSN: 0168-1923