Articles | Volume 13, issue 6
https://doi.org/10.5194/amt-13-2923-2020
https://doi.org/10.5194/amt-13-2923-2020
Research article
 | 
05 Jun 2020
Research article |  | 05 Jun 2020

Correcting high-frequency losses of reactive nitrogen flux measurements

Pascal Wintjen, Christof Ammann, Frederik Schrader, and Christian Brümmer

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Cited articles

Ammann, C.: On the applicability of relaxed eddy accumulation and common methods for measuring trace gas fluxes, PhD thesis, ETH Zurich, https://doi.org/10.3929/ethz-a-002031554, 1999 a, b, c, d, e, f, g, h, i, j
Ammann, C., Brunner, A., Spirig, C., and Neftel, A.: Technical note: Water vapour concentration and flux measurements with PTR-MS, Atmos. Chem. Phys., 6, 4643–4651, https://doi.org/10.5194/acp-6-4643-2006, 2006. a, b, c, d
Ammann, C., Wolff, V., Marx, O., Brümmer, C., and Neftel, A.: Measuring the biosphere-atmosphere exchange of total reactive nitrogen by eddy covariance, Biogeosciences, 9, 4247–4261, https://doi.org/10.5194/bg-9-4247-2012, 2012. a, b, c, d, e, f
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Aubinet, M., Vesala, T., and Papale, D. (Eds.): Eddy Covariance: A Practical Guide to Measurement and Data Analysis, Springer Science+Business Media B.V., Dordrecht, The Netherlands, 2012. a, b, c, d, e, f, g, h
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Short summary
With recent technological advances it is now possible to measure the exchange of trace gases between the land surface and the atmosphere. When using the so-called eddy-covariance method, certain corrections need to be applied to account for attenuation in the flux signal. These losses were found to be setup- and site-specific and can be up to 38 % for reactive nitrogen fluxes. We evaluated five different methods and recommend using an empirical version with locally measured cospectra.
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