Nitrous oxide emissions 1999 to 2009 from a global atmospheric inversion
N[subscript 2]O surface fluxes were estimated for 1999 to 2009 using a time-dependent Bayesian inversion technique. Observations were drawn from 5 different networks, incorporating 59 surface sites and a number of ship-based measurement series. To avoid biases in the inverted fluxes, the data were a...
| Main Authors: | , , , , , , , , , , , , , , |
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| Other Authors: | |
| Format: | Article |
| Language: | en_US |
| Published: |
Copernicus GmbH
2014
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| Online Access: | http://hdl.handle.net/1721.1/87566 https://orcid.org/0000-0001-5925-3801 |
| Summary: | N[subscript 2]O surface fluxes were estimated for 1999 to 2009 using a time-dependent Bayesian inversion technique. Observations were drawn from 5 different networks, incorporating 59 surface sites and a number of ship-based measurement series. To avoid biases in the inverted fluxes, the data were adjusted to a common scale and scale offsets were included in the optimization problem. The fluxes were calculated at the same resolution as the transport model (3.75° longitude × 2.5° latitude) and at monthly time resolution. Over the 11-year period, the global total N[subscript 2]O source varied from 17.5 to 20.1 Tg a[superscript −1] N. Tropical and subtropical land regions were found to consistently have the highest N[subscript 2]O emissions, in particular in South Asia (20 ± 3% of global total), South America (13 ± 4%) and Africa (19 ± 3%), while emissions from temperate regions were smaller: Europe (6 ± 1%) and North America (7 ± 2%). A significant multi-annual trend in N[subscript 2]O emissions (0.045 Tg a[superscript −2] N) from South Asia was found and confirms inventory estimates of this trend. Considerable interannual variability in the global N[subscript 2]O source was observed (0.8 Tg a[superscript −1] N, 1 standard deviation, SD) and was largely driven by variability in tropical and subtropical soil fluxes, in particular in South America (0.3 Tg a[superscript −1] N, 1 SD) and Africa (0.3 Tg a[superscript −1] N, 1 SD). Notable variability was also found for N[subscript 2]O fluxes in the tropical and southern oceans (0.15 and 0.2 Tg a[superscript −1] N, 1 SD, respectively). Interannual variability in the N[subscript 2]O source shows some correlation with the El Niño–Southern Oscillation (ENSO), where El Niño conditions are associated with lower N[subscript 2]O fluxes from soils and from the ocean and vice versa for La Niña conditions. |
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