Radiative forcing since preindustrial times due to ozone change in the troposphere and the lower stratosphere

Changes in atmospheric ozone have occurred since the preindustrial era as a result of increasing anthropogenic emissions. Within ACCENT, a European Network of Excellence, ozone changes between 1850 and 2000 are assessed for the troposphere and the lower stratosphere (up to 30 km) by a variety of sev...

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Wedi'i Gadw mewn:
Manylion Llyfryddiaeth
Prif Awduron: M. Gauss, G. Myhre, I. S. A. Isaksen, V. Grewe, G. Pitari, O. Wild, W. J. Collins, F. J. Dentener, K. Ellingsen, L. K. Gohar, D. A. Hauglustaine, D. Iachetti, F. Lamarque, E. Mancini, L. J. Mickley, M. J. Prather, J. A. Pyle, M. G. Sanderson, K. P. Shine, D. S. Stevenson, K. Sudo, S. Szopa, G. Zeng
Fformat: Artigo
Iaith:Inglês
Cyhoeddwyd: Copernicus Publications 2006-01-01
Cyfres:Atmospheric Chemistry and Physics
Mynediad Ar-lein:http://www.atmos-chem-phys.net/6/575/2006/acp-6-575-2006.pdf
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