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Autor:
Martin Graus, M. Martin, B. Sierau, Carlton D. Rauschenberg, Armin Hansel, Q. Gao, M. Westberg, L. Di Liberto, Michael Tjernström, M. Szczodrak, Joseph Sedlar, P. O. G. Persson, Erik Swietlicki, E. Granath, G. de Leeuw, Mónica V. Orellana, Petri Vaattovaara, Johan Knulst, D. Orsini, Markus Müller, Zoran Ristovski, C. R. Wheeler, Ian M. Brooks, N. Wahlberg, Matthew D. Shupe, Rachel Y.-W. Chang, Caroline Leck, Jan W. Bottenheim, S. Sjogren, Thorsten Mauritsen, Jussi Paatero, Olaf Stetzer, Paul E. Johnston, Barbara Brooks, Andrew J. Hind, Leif Backlin, Cathryn E. Birch, Sarah J. Norris, Andreas Held, Patricia A. Matrai, S. de la Rosa, Anders Sirevaag, Jost Heintzenberg
Publikováno v:
Atmospheric Chemistry and Physics, 6, 14, 2823-2869
Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics, 14 (6)
Atmospheric Chemistry and Physics, Vol 14, Iss 6, Pp 2823-2869 (2014)
Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics, 14 (6)
Atmospheric Chemistry and Physics, Vol 14, Iss 6, Pp 2823-2869 (2014)
The climate in the Arctic is changing faster than anywhere else on earth. Poorly understood feedback processes relating to Arctic clouds and aerosol–cloud interactions contribute to a poor understanding of the present changes in the Arctic climate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::32efdc33278fd41ffb42d1e9744450c8
http://resolver.tudelft.nl/uuid:cf3093e1-40ce-477c-bb91-ed53ed7ed870
http://resolver.tudelft.nl/uuid:cf3093e1-40ce-477c-bb91-ed53ed7ed870