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EOS MLS observations of ozone loss in the 2004–2005 Arctic winter
Author(s) -
Manney G. L.,
Santee M. L.,
Froidevaux L.,
Hoppel K.,
Livesey N. J.,
Waters J. W.
Publication year - 2006
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2005gl024494
Subject(s) - microwave limb sounder , vortex , chemical transport model , atmospheric sciences , arctic , polar vortex , environmental science , stratosphere , ozone , ozone depletion , sudden stratospheric warming , climatology , the arctic , geology , meteorology , oceanography , physics , troposphere
Earth Observing System Microwave Limb Sounder O 3 and N 2 O are used to examine transport and chemical O 3 loss in the unusually cold 2004–2005 Arctic winter. The vortex was dynamically active, with episodic mixing events throughout the winter; descent was the dominant transport process only through late January. Before the onset of lower stratospheric chemical loss, O 3 was higher near the vortex edge than in the vortex core, causing different effects of mixing depending on the vortex region and time, either masking or mimicking chemical loss. O 3 loss ceased by 10 March because of an early final warming. Rough estimates suggest maximum vortex‐averaged O 3 loss of 1.2–1.5 ppmv between 450 and 500 K, with up to ∼2 ppmv loss in the outer vortex near 500 K. Despite record cold, chemical O 3 loss was less in 2004–2005 than in previous cold Arctic winters.