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Designing an observation strategy for N2O

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Freibauer,  A.
Department Biogeochemical Processes, Prof. E.-D. Schulze, Max Planck Institute for Biogeochemistry, Max Planck Society;

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Citation

Freibauer, A. (2008). Designing an observation strategy for N2O. In A. J. Dolman, A. Freibauer, & R. Valentini (Eds.), The continental-scale greenhouse gas balance of europe (pp. 135-151). New York [u.a.]: Springer.


Cite as: https://hdl.handle.net/11858/00-001M-0000-000E-D66E-5
Abstract
Nitrous oxide (N2O) is a powerful greenhouse gas (GHG) with a global warming potential (GWP) of 296 in relation to CO2 (IPCC 2001). In the context of the United Nations Framework Convention on Climate Change (UNFCCC), a GWP value of 310 is used (IPCC 1996). For easy comparison, we express N2O fluxes in units of nitrogen (N) and in CO2-carbon equivalents (Ceq), applying the politically relevant GWP of 310 (Eq. 8.1). N2O is also involved in the depletion of the stratospheric ozone layer. This chapter will give an overview of the present N2O emissions in Europe, and then focus on the major source, the soilborne N2O emissions. The spatio-temporal variation of soil N2O fluxes and underlying biogoechemical processes will be described, as well as approaches to observe and quantify N2O fluxes, associated uncertainties and ways towards a systematic operational N2O monitoring. In the latter part, N2O emissions from other sources than soils will be included.