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The fluxes were calculated at the same resolution as the transport model (3.75° longitude × 2.5° latitude) and at monthly time resolution. To avoid biases in the inverted fluxes, the data were adjusted to a common scale and scale offsets were included in the optimization problem. Observations were drawn from 5 different networks, incorporating 59 surface sites and a number of ship-based measurement series. N 2O surface fluxes were estimated for 1999 to 2009 using a time-dependent Bayesian inversion technique. Hide author details Received: – Discussion started: – Revised: – Accepted: – Published: Ībstract. 11 Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA.10 Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan.9 Atmospheric Chemistry Research Group, School of Chemistry, University of Bristol, Bristol, UK.8 Center for Atmospheric and Oceanic Studies, Graduate School of Science, Tohoku University, Sendai 980-8578, Japan.
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7 National Institute for Environmental Studies, Tsukuba, Japan.6 Scripps Institution of Oceanography, La Jolla, CA, USA.5 Center for Global Change Science, MIT, Cambridge, MA, USA.4 Commonwealth Scientific and Industrial Research Organisation, Aspendale, Australia.3 NOAA ESRL, Global Monitoring Division, Boulder, CO, USA.2 Laboratoire des Sciences du Climat et de l'Environnement, Gif sur Yvette, France.1 Norwegian Institute for Air Research, Kjeller, Norway.