Early unusual ozone loss during the Arctic winter 2002/2003 compared to other winters

International audience 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...

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Bibliographic Details
Main Authors: Goutail, Florence, Pommereau, Jean-Pierre, Lefèvre, Franck, van Roozendael, M., Andersen, S. B., Kåstad Hoiskar, B. A., Dorokhov, V., Kyrö, E., Chipperfield, M. P., Feng, W.
Other Authors: Service d'aéronomie (SA), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Belgian Institute for Space Aeronomy / Institut d'Aéronomie Spatiale de Belgique (BIRA-IASB), Danish Meteorological Institute (DMI), Norwegian Institute for Air Research (NILU), Central Aerological Observatory (CAO), Russian Federal Service for Hydrometeorology and Environmental Monitoring (Roshydromet), Finnish Meteorological Institute (FMI), School of Earth and Environment Leeds (SEE), University of Leeds
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2004
Subjects:
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
Arctic
Online Access:https://hal.science/hal-00327910
https://hal.science/hal-00327910/document
https://hal.science/hal-00327910/file/acpd-4-5019-2004.pdf
Description
Summary:International audience 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.

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