Simulations of cosmogenic super(1) super(4) CO using the three-dimensional atmospheric model MATCH: effects of super(1) super(4) C production distribution and the solar cycle

Most atmospheric super(1) super(4) CO is produced by cosmic rays in the lowermost stratosphere and upper troposphere. The main removal process for super(1) super(4) CO is oxidation by OH radicals. Assuming that the spatial distribution of OH is well known, super(1) super(4) CO can be useful as a tes...

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Veröffentlicht in:	Journal of Geophysical Research, Washington, DC Washington, DC, 1999-01, Vol.104 (D9), p.11733-11743
Hauptverfasser:	Joeckel, Patrick, Lawrence, Mark G, Brenninkmeijer, Carl AM
Format:	Artikel
Sprache:	eng
Online-Zugang:	Volltext
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