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Martin D., Tsivou M., Bonsang B., Abonnel C., Carsey T.P. & Springer Young M. (1997). Hydrogen peroxide (H2O2) in the marine atmospheric boundary layer during the ASTEX/MAGE experiment in the eastern subtropical North Atlantic. J. Geophys. Res., 102, 6003–6015.
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Heikkila U., Beer J., Jouzel J., Feitcher J., Kubik P. (2008). Be-10 measured in a GRIP snow pit and modeled using the ECHAM5-HAM general circulation model. Geophysical research letters, 35, L05817.
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Ruth U., C. Barbante, M. Bigler, B. Delmonte, H. Fischer, P. Gabrielli, V. Gaspari, P. Kaufmann, F. Lambert, V. Maggi, F. Marino, J.R. Petit, J.P. Steffensen, R. Traversi, R. Udisti, D. Wagenbach, A. Wegner, E. Wolff. (2008). Proxies and measurement techniques for mineral dust in Antarctic ice cores. Environ. Sci. Technol., 42, 5675–5681.
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Kerminen V.M., Hillamo R., Makela T., Jaffrezo J.L., . & Maenhaut W. (1998). The physicochemical structure of the Greenland summer aerosol and its relation to atmospheric processes. J. Geophys. Res., 103(d5), 5661–5670.
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Bulat, S., Alekhina, I., Petit, J.R., Steffensen J.P., Dahl-Jensen, D. (2005). Bacteria and archaea under Greenland ice sheet: NGRIP ‘red’ ice issue. (Vol. 7).
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Bulat, S. Alekhina, I., Lipenkov, V.Y., Lukin, V., Marie, D., Petit, J.R. (2005). Deliberations on microbial life in the subglacial Lake Vostok, East Antarctica. (Vol. 7).
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La Chapelle S., Castelnau O., Lipenkov V.Y. & Duval P. (1998). Dynamic recrystallization and texture development in ice as revealed by the study of deep ice cores in Antarctica and Greenland. J. Geophys. Res., 103(b3), 5091–5105.
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Goutail, F., J.-P. Pommereau, F. Lefèvre, M. Van Roozendael, S. B. Andersen, B.-A. Kåstad Høiskar, V. Dorokhov, E. Kyro, M. P. Chipperfield and W. Feng. (2004). Early unusual ozone loss during the Arctic winter 2002/03 compared to other winters. Atmospheric chemistry and physics, 4, 5019–5044.
Abstract: Total column ozone reduction in the Arctic is evaluated each winter since 1993/1994 by the transport method (3-D CTM passive ozone minus measurements). The cumulative loss from 1 December to the end of the season ranges from 5–10% during warm winters like 1998/1999, 2000/2001 and 2001/2002 up to 30%–32% during cold winters like 1994/1995 and 1995/1996. The 23% cumulative loss observed during the winter 2002/2003 is similar in amplitude to the 20–24% measured in 1996/1997 and 1999/2000 but the timing is different. It started unusually early in December after the occurrence of very low temperature at all stratospheric levels between 550 K and 435 K allowing PSC formation and thus chlorine activation. The early ozone loss of 2002/2003 is well captured by current 3-D CTM models.
Programme: 904
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Zorn, S.R.; Drewnick, F.; Schott, M.; Hoffmann, T.; Borrmann, S. (2008). Characterization of the South Atlantic marine boundary layer aerosol using an aerodyne aerosol mass spectrometer. Atmospheric chemistry and physics, 8(16), 4711–4728.
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Brossard T., Elvebakk A., Joly D. & Nilsen L. (2002). Modelling index of thermophily by means of a multi-sources data base on Brogger Peninsula (Svalbard). International journal of remote sensing, 23(21), 4683–4698.
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