Regional N<sub>2</sub>O fluxes in Amazonia derived from aircraft vertical profiles
Nitrous oxide (N<sub>2</sub>O) is the third most important anthropogenic greenhouse gas. Globally, the main sources of N<sub>2</sub>O are nitrification and denitrification in soils. About two thirds of the soil emissions occur in the tropics and approximately 20% originate in...
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doaj-c4b840c3d2a54bd0996a86b5a3c202dd2020-11-24T23:05:08ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242009-11-0192287858797Regional N<sub>2</sub>O fluxes in Amazonia derived from aircraft vertical profilesP. TansJ. B. MillerM. T. S. D'AmelioL. V. GattiNitrous oxide (N<sub>2</sub>O) is the third most important anthropogenic greenhouse gas. Globally, the main sources of N<sub>2</sub>O are nitrification and denitrification in soils. About two thirds of the soil emissions occur in the tropics and approximately 20% originate in wet rainforest ecosystems, like the Amazon forest. The work presented here involves aircraft vertical profiles of N<sub>2</sub>O from the surface to 4 km over two sites in the Eastern and Central Amazon: Tapajós National Forest (SAN) and Cuieiras Biologic Reserve (MAN), and the estimation of N<sub>2</sub>O fluxes for regions upwind of these sites. To our knowledge, these regional scale N<sub>2</sub>O measurements in Amazonia are unique and represent a new approach to looking regional scale emissions. The fluxes upwind of MAN exhibited little seasonality, and the annual mean was 2.1±1.0 mg N<sub>2</sub>O m<sup>−2</sup> day<sup>−1</sup>, higher than that for fluxes upwind of SAN, which averaged 1.5±1.6 mg N<sub>2</sub>O m<sup>−2</sup> day<sup>−1</sup>. The higher rainfall around the MAN site could explain the higher N<sub>2</sub>O emissions, as a result of increased soil moisture accelerating microbial nitrification and denitrification processes. For fluxes from the coast to SAN seasonality is present for all years, with high fluxes in the months of March through May, and in November through December. The first peak of N<sub>2</sub>O flux is strongly associated with the wet season. The second peak of high N<sub>2</sub>O flux recorded at SAN occurs during the dry season and can not be easily explained. However, about half of the dry season profiles exhibit significant correlations with CO, indicating a larger than expected source of N<sub>2</sub>O from biomass burning. The average CO:N<sub>2</sub>O ratio for all profiles sampled during the dry season is 94±77 mol CO:mol N<sub>2</sub>O and suggests a larger biomass burning contribution to the global N<sub>2</sub>O budget than previously reported. http://www.atmos-chem-phys.net/9/8785/2009/acp-9-8785-2009.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
P. Tans J. B. Miller M. T. S. D'Amelio L. V. Gatti |
spellingShingle |
P. Tans J. B. Miller M. T. S. D'Amelio L. V. Gatti Regional N<sub>2</sub>O fluxes in Amazonia derived from aircraft vertical profiles Atmospheric Chemistry and Physics |
author_facet |
P. Tans J. B. Miller M. T. S. D'Amelio L. V. Gatti |
author_sort |
P. Tans |
title |
Regional N<sub>2</sub>O fluxes in Amazonia derived from aircraft vertical profiles |
title_short |
Regional N<sub>2</sub>O fluxes in Amazonia derived from aircraft vertical profiles |
title_full |
Regional N<sub>2</sub>O fluxes in Amazonia derived from aircraft vertical profiles |
title_fullStr |
Regional N<sub>2</sub>O fluxes in Amazonia derived from aircraft vertical profiles |
title_full_unstemmed |
Regional N<sub>2</sub>O fluxes in Amazonia derived from aircraft vertical profiles |
title_sort |
regional n<sub>2</sub>o fluxes in amazonia derived from aircraft vertical profiles |
publisher |
Copernicus Publications |
series |
Atmospheric Chemistry and Physics |
issn |
1680-7316 1680-7324 |
publishDate |
2009-11-01 |
description |
Nitrous oxide (N<sub>2</sub>O) is the third most important anthropogenic greenhouse gas. Globally, the main sources of N<sub>2</sub>O are nitrification and denitrification in soils. About two thirds of the soil emissions occur in the tropics and approximately 20% originate in wet rainforest ecosystems, like the Amazon forest. The work presented here involves aircraft vertical profiles of N<sub>2</sub>O from the surface to 4 km over two sites in the Eastern and Central Amazon: Tapajós National Forest (SAN) and Cuieiras Biologic Reserve (MAN), and the estimation of N<sub>2</sub>O fluxes for regions upwind of these sites. To our knowledge, these regional scale N<sub>2</sub>O measurements in Amazonia are unique and represent a new approach to looking regional scale emissions. The fluxes upwind of MAN exhibited little seasonality, and the annual mean was 2.1±1.0 mg N<sub>2</sub>O m<sup>−2</sup> day<sup>−1</sup>, higher than that for fluxes upwind of SAN, which averaged 1.5±1.6 mg N<sub>2</sub>O m<sup>−2</sup> day<sup>−1</sup>. The higher rainfall around the MAN site could explain the higher N<sub>2</sub>O emissions, as a result of increased soil moisture accelerating microbial nitrification and denitrification processes. For fluxes from the coast to SAN seasonality is present for all years, with high fluxes in the months of March through May, and in November through December. The first peak of N<sub>2</sub>O flux is strongly associated with the wet season. The second peak of high N<sub>2</sub>O flux recorded at SAN occurs during the dry season and can not be easily explained. However, about half of the dry season profiles exhibit significant correlations with CO, indicating a larger than expected source of N<sub>2</sub>O from biomass burning. The average CO:N<sub>2</sub>O ratio for all profiles sampled during the dry season is 94±77 mol CO:mol N<sub>2</sub>O and suggests a larger biomass burning contribution to the global N<sub>2</sub>O budget than previously reported. |
url |
http://www.atmos-chem-phys.net/9/8785/2009/acp-9-8785-2009.pdf |
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