Prolonged stratospheric ozone loss in the 1995/96 Arctic winter

• Main Authors: Rex, Markus, Harris, N. R. P., von der Gathen, Peter, Lehmann, Ralph, Braathen, G. O., Reimer, E., Beck, A., Chipperfield, M. P., Alfier, R., Allaart, M., O'Connor, F., Dier, H., Dorokhov, V., Fast, H., Gil, M., Kyrö, E., Litynska, Z., Mikkelsen, I. S., Molyneux, M. G., Nakane, H., Notholt, Justus, Rummukainen, M., Viatte, P., Wenger, J.
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: 1997
• Subjects: Antarctic; Arctic; The Antarctic; Antarc*
• Online Access: https://epic.awi.de/id/eprint/2572/; https://hdl.handle.net/10013/epic.13157

It is well established that extensive depletion of ozone, initiated by heterogenous reactions on polar stratospheric clouds(PSCs) can occur in both the Arctic and Antarctic lower stratosphere. Moreover, it has been shown that ozone lossrates in the Arctic region in recent years reached values comparable to those over the Antarctic. But until now theaccumulated ozone losses over the Arctic have been the smaller, mainly because the period of Arctic ozone loss hasnot-unlike over the Antarctic-persisted well into springtime. Here we report the occurrence-during the unusuallycold 1995-96 Arctic winter-of the highest recorded chemical ozone loss over the Arctic region. Two new kinds ofbehaviour were observed. First, ozone loss at some altitudes was observed long after the last exposure to PSCs. Thiscontinued loss appears to be due to a removal of the nitrogen species that slow down chemical ozone depletion. Second,in another altitude range ozone loss rates decreased while PSCs were still present, apparently because of an earlytransformation of the ozone-destroying chlorine species into less active chlorinenitrate. The balance between these twocounteracting mechanisms is probably a fine one, determined by small differences in wintertime stratospherictemperatures. If the apparent cooling trend in the Arctic stratosphere is real, more dramatic ozone losses may occurin the future.