[1] Arctic denitrification in the winter 2004/2005 is analyzed using measurements from the satellite instrument ACE-FTS. Two methods based on changes in the correlations of odd nitrogen (NOy) versus methane and versus an artificial long-lived tracer are employed. The observations show that significa...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.663.1733 2023-05-15T15:01:05+02:00 Respectively. Citation Jin K. Semeniuk G. L. Manney The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.663.1733 http://www.ace.uwaterloo.ca/publications/2006/Jin-Denitrificationt2006reprint.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.663.1733 http://www.ace.uwaterloo.ca/publications/2006/Jin-Denitrificationt2006reprint.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.ace.uwaterloo.ca/publications/2006/Jin-Denitrificationt2006reprint.pdf text ftciteseerx 2016-01-08T16:58:08Z [1] Arctic denitrification in the winter 2004/2005 is analyzed using measurements from the satellite instrument ACE-FTS. Two methods based on changes in the correlations of odd nitrogen (NOy) versus methane and versus an artificial long-lived tracer are employed. The observations show that significant denitrification occurred in the region 15 km–20 km and that it was spatially inhomogeneous within the polar vortex. Before the vortex breakup inmid-March 2005 amaximumdenitrification of 8 ± 0.8 ppbv, accounting for a relative reduction of over 50%,was observed at 450 K (17 km) using both methods. When averaged over the polar vortex for the first half of March, the denitrification at this level was about 4.4 ppbv and 5.0 ppbv from the artificial tracer method and the correlation method Text Arctic Unknown Arctic |
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[1] Arctic denitrification in the winter 2004/2005 is analyzed using measurements from the satellite instrument ACE-FTS. Two methods based on changes in the correlations of odd nitrogen (NOy) versus methane and versus an artificial long-lived tracer are employed. The observations show that significant denitrification occurred in the region 15 km–20 km and that it was spatially inhomogeneous within the polar vortex. Before the vortex breakup inmid-March 2005 amaximumdenitrification of 8 ± 0.8 ppbv, accounting for a relative reduction of over 50%,was observed at 450 K (17 km) using both methods. When averaged over the polar vortex for the first half of March, the denitrification at this level was about 4.4 ppbv and 5.0 ppbv from the artificial tracer method and the correlation method |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Respectively. Citation Jin K. Semeniuk G. L. Manney |
spellingShingle |
Respectively. Citation Jin K. Semeniuk G. L. Manney |
author_facet |
Respectively. Citation Jin K. Semeniuk G. L. Manney |
author_sort |
Respectively. Citation Jin |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.663.1733 http://www.ace.uwaterloo.ca/publications/2006/Jin-Denitrificationt2006reprint.pdf |
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Arctic |
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http://www.ace.uwaterloo.ca/publications/2006/Jin-Denitrificationt2006reprint.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.663.1733 http://www.ace.uwaterloo.ca/publications/2006/Jin-Denitrificationt2006reprint.pdf |
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