The importance of dissolved organic carbon fluxes for the carbon balance of a temperate Scots pine forest. Agricultural and Forest Meteorology, Bellassen, V.
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Reconstruction and attribution of the carbon sink of European forests between and Potential knowledge gain in large-scale simulations of forest carbon fluxes from remotely sensed biomass and height. Forest Ecology and Management, Anderson, et al. Biophysical considerations in forestry for climate protection. Frontiers in Ecology and the Environment, Schwalm, C. Schulze, E. Part 4: integration of carbon and other trace-gas fluxes. Part 4: integration of carbon and other trace-gas fluxes vol 16, pg , Richardson, A. Piao, S. Ecology, Part 3: forests.
Plos One, Janssens, I. Dieleman W.
Plant Cell and Environment, Ciais, P. Part 2: croplands. Can we reconcile atmospheric estimates of the Northern terrestrial carbon sink with land-based accounting?
Beer, C. Science, Luyssaert, Nitrogen's carbon bonus. Battin, T. Ecological Informatics, Jung, M. To date, relatively few such studies have been undertaken in the arctic due to the harsh environmental conditions and difficult access to remote locations. Continuous monitoring at locations with limited solar power availability in winter and where wind power is not a viable option requires selecting robust sensors with extremely low power requirements, and remote system-diagnostic capabilities.
The very low power consumption of the EC proved especially beneficial over the winter months when solar power was limited.
For these types of northern applications, periodic generator charges are often required during the darkest winter months. Another advantage of the EC that makes it a good choice for cold, remote locations is the self-regulating temperature control of the EC, which protects the inner parts of the analyzer in extreme cold while maximizing power-use efficiency. Data collected from the Bonanza Creek sites includes fluxes of atmospheric carbon dioxide, water vapor, surface energy, photosynthetically active radiation, air and soil temperatures, rainfall, snow depth, soil moisture content, wind direction and speed, and average atmospheric concentrations of CO 2 and H 2 O throughout the year.
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