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Evidence for a CO increase in the SH during the 20th century based on firn air samples from Berkner Island, Antarctica

MPS-Authors
http://pubman.mpdl.mpg.de/cone/persons/resource/persons100836

Assonov,  S. S.
Atmospheric Chemistry, Max Planck Institute for Chemistry, Max Planck Society;

http://pubman.mpdl.mpg.de/cone/persons/resource/persons100865

Brenninkmeijer,  C. A. M.
Atmospheric Chemistry, Max Planck Institute for Chemistry, Max Planck Society;

http://pubman.mpdl.mpg.de/cone/persons/resource/persons101035

Jöckel,  P. J.
Atmospheric Chemistry, Max Planck Institute for Chemistry, Max Planck Society;

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Citation

Assonov, S. S., Brenninkmeijer, C. A. M., Jöckel, P. J., Mulvaney, R., Bernard, S., & Chappellaz, J. (2007). Evidence for a CO increase in the SH during the 20th century based on firn air samples from Berkner Island, Antarctica. Atmospheric Chemistry and Physics, 7, 295-308.


Cite as: http://hdl.handle.net/11858/00-001M-0000-0014-8757-D
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