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1.	Juday, G.P, et al. (author) Chapter 14: Forests, Land Management and Agriculture 2005 In: The Arctic Climate Impact Assessment - The Scientific Report. - Cambridge : Cambridge University Press. - 0521865093 ; , s. 781-862 Book chapter (other academic/artistic)
2.	Tchebakova, N. M., et al. (author) Energy and Mass Exchange and the Productivity of Main Siberian Ecosystems (from Eddy Covariance Measurements). 1. Heat Balance Structure over the Vegetation Season 2015 In: Biology Bulletin of the Russian Academy of Science. - 1062-3590. ; 42:6, s. 570-578 Journal article (peer-reviewed)abstract Direct measurements of heat balance (latent heat and sensible heat fluxes) by the eddy covariance method, undertaken in 1998-2000 and 2002-2004, are used to obtain information on the daily, seasonal, and annual dynamics of energy and mass exchange between the atmosphere and the typical ecosystems of Siberia (middle taiga pine forest, raised bog, and true four grass steppe with data for typical tundra) along the Yenisei meridian (90 degrees E).
3.	Tchebakova, N. M., et al. (author) Energy and Mass Exchange and the Productivity of Main Siberian Ecosystems (from Eddy Covariance Measurements). 2. Carbon Exchange and Productivity 2015 In: Biology Bulletin of the Russian Academy of Science. - 1062-3590. ; 42:6, s. 579-588 Journal article (peer-reviewed)abstract Direct measurements of CO2 fluxes by the eddy covariance method have demonstrated that the examined middle-taiga pine forest, raised bog, true steppe, and southern tundra along the Yenisei meridian (similar to 90 degrees E) are carbon sinks of different capacities according to annual output. The tundra acts as a carbon sink starting from June; forest and bog, from May; and steppe, from the end of April. In transitional seasons and winter, the ecosystems are a weak source of carbon; this commences from September in the tundra, from October in the forest and bog, and from November in the steppe. The photosynthetic productivity of forest and steppe ecosystems, amounting to 480-530 g C/(m(2) year), exceeds by 2-2.5 times that of bogs and tundras, 200-220 g C/(m(2) year). The relationships between the heat balance structure and CO2 exchange are shown. Possible feedback of carbon exchange between the ecosystems and atmosphere as a result of climate warming in the region are assessed.

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Type of publication: journal article (2); book chapter (1)

Type of content: peer-reviewed (2); other academic/artistic (1)

Author/Editor: Tchebakova, N.M. (3); Arneth, Almut (2); Schulze, E-D (2); Valentini, R. (2); Vaganov, E. A. (2); Marchesini, L. Belel ... (2); show more...; Vygodskaya, N. N. (2); Kurbatova, Yu. A. (2); Parfenova, E. I. (2); Linderholm, Hans W., ... (1); Linder, S (1); Kolle, O. (1); Berg, E (1); D'Arrigo, R. (1); Kirdyanov, A. V. (1); Wilmking, M. (1); Duffy, P. (1); Eggertsson, O. (1); Lewis, C. E. (1); Kellomaki, S. (1); Juday, G.P (1); Barber, V (1); Rupp, S (1); Sparrow, S (1); Vaganov, E (1); Yarie, J (1); Furyaev, V.V (1); Hogg, E.H. (1); Huttunen, S (1); Jacoby, G (1); Kaplunov, V.Y. (1); Naurzbaev, M.M. (1); Pleshikov, F.I. (1); Runesson, U.T. (1); Savva, Y.V. (1); Sidorova, O.V. (1); Stakanov, V.D. (1); Valendik, E.F. (1); Vedrova, E.F. (1); Verkhovets, S. V. (1); show less...

University: Lund University (2); University of Gothenburg (1)

Language: English (3)

Research subject (UKÄ/SCB): Natural sciences (3)

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