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Observations of total RONO<sub>2</sub> over the boreal forest: NO<sub>x</sub> sinks and HNO<sub>3</sub> sources

In contrast with the textbook view of remote chemistry where HNO<sub>3</sub> formation is the primary sink of nitrogen oxides, recent theoretical analyses show that formation of RONO<sub>2</sub> (&Sigma;ANs) from isoprene and other terpene precursors is the primary net chemical loss of nitrogen oxid...

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I tiakina i:
Ngā taipitopito rārangi puna kōrero
Ngā kaituhi matua: E. C. Browne, K.-E. Min, P. J. Wooldridge, E. Apel, D. R. Blake, W. H. Brune, C. A. Cantrell, M. J. Cubison, G. S. Diskin, J. L. Jimenez, A. J. Weinheimer, P. O. Wennberg, A. Wisthaler, R. C. Cohen
Hōputu: Artigo
Reo:Inglês
I whakaputaina: Copernicus Publications 2013-05-01
Rangatū:Atmospheric Chemistry and Physics
Urunga tuihono:http://www.atmos-chem-phys.net/13/4543/2013/acp-13-4543-2013.pdf
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