Carbon dioxide balance of subarctic tundra from plot to regional scales

We report here the carbon dioxide (CO 2 ) budget of a 98.6 km 2 subarctic tundra area in northeast European Russia based on measurements at two different scales and two independent upscaling approaches. Plot-scale measurements (chambers on terrestrial surfaces, gas gradient method and bubble collect...

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Bibliographic Details
Published in:Biogeosciences
Main Authors: Marushchak, M. E., Kiepe, I., Biasi, C., Elsakov, V., Friborg, T., Johansson, T., Soegaard, H., Virtanen, T., Martikainen, P. J.
Format: Text
Language:English
Published: 2018
Subjects:
Subarctic
Tundra
Online Access:https://doi.org/10.5194/bg-10-437-2013
https://www.biogeosciences.net/10/437/2013/
Description
Summary:We report here the carbon dioxide (CO 2 ) budget of a 98.6 km 2 subarctic tundra area in northeast European Russia based on measurements at two different scales and two independent upscaling approaches. Plot-scale measurements (chambers on terrestrial surfaces, gas gradient method and bubble collectors on lakes) were carried out from July 2007 to October 2008. The landscape-scale eddy covariance (EC) measurements covered the snow-free period of 2008. The annual net ecosystem exchange (NEE) of different land cover types ranged from −251 to 84 g C m −2 . Leaf area index (LAI) was an excellent predictor of the spatial variability in gross photosynthesis (GP), NEE and ecosystem respiration (ER). The plot-scale CO 2 fluxes were first scaled up to the EC source area and then to the whole study area using two data sets: a land cover classification and a LAI map, both based on field data and a 2.4 m pixel-sized QuickBird satellite image. The good agreement of the CO 2 balances for the EC footprint based on the different measuring techniques (−105 to −81 g C m −2 vs. −79 g C m −2 growing season 2008) justified the integration of the plot-scale measurements over the larger area. The regional CO 2 balance based on area-integrated plot-scale measurements was −41 or −79 g C m −2 yr −1 according to the two upscaling methods, the land cover classification and the LAI map, respectively. Due to the heterogeneity of tundra, the effect of climate change on CO 2 uptake will vary strongly according to the land cover type and, moreover, likely changes in their relative coverage in the future will have great impact on the regional CO 2 balance.

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