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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., Montagnani, L., Rebmann, C., Sedlak, P., & Van Gorsel, E. (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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資料種別: 学術論文

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BGC1350.pdf (出版社版), 888KB
 
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BGC1350.pdf
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 作成者:
Aubinet, M., 著者
Feigenwinter, C., 著者
Heinesch, B., 著者
Bernhöfer, C., 著者
Canepa, E., 著者
Lindroth, A., 著者
Montagnani, L., 著者
Rebmann, C.1, 著者           
Sedlak, P., 著者
Van Gorsel, E., 著者
所属:
1Department Biogeochemical Processes, Prof. E.-D. Schulze, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1497751              

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キーワード: 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
 要旨: 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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言語: eng - English
 日付: 2010
 出版の状態: 出版
 ページ: -
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 査読: -
 識別子(DOI, ISBNなど): DOI: 10.1016/j.agrformet.2010.01.016
ISI: ://000278244400002
その他: BGC1350
 学位: -

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出版物 1

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出版物名: Agricultural and Forest Meteorology
種別: 学術雑誌
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出版社, 出版地: Amsterdam : Elsevier
ページ: - 巻号: 150 (5) 通巻号: - 開始・終了ページ: 655 - 664 識別子(ISBN, ISSN, DOIなど): CoNE: https://pure.mpg.de/cone/journals/resource/954928468040
ISSN: 0168-1923