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The northern hemisphere stratospheric vortex during the 2002–03 winter: Subsidence, chlorine activation and ozone loss observed by the Odin Sub‐Millimetre Radiometer
Author(s) -
Urban J.,
Lautié N.,
Le Flochmoën E.,
Murtagh D.,
Ricaud P.,
De La Noë J.,
Dupuy E.,
Drouin A.,
El Amraoui L.,
Eriksson P.,
Frisk U.,
Jiménez C.,
Kyrölä E.,
Llewellyn E. J.,
Mégie G.,
Nordh L.,
Olberg M.
Publication year - 2004
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 - 10.1029/2003gl019089
Subject(s) - ozone , polar vortex , radiometer , atmospheric sciences , northern hemisphere , stratosphere , environmental science , subsidence , ozone layer , arctic , ozone depletion , microwave limb sounder , southern hemisphere , depth sounding , climatology , meteorology , geology , oceanography , physics , remote sensing , paleontology , structural basin
We present profile measurements of key constituents relevant to stratospheric chemistry and dynamics such as ozone (O 3 ), nitrous oxide (N 2 O), and chlorine monoxide (ClO) taken during the 2002–03 northern hemisphere winter by the Odin Sub‐Millimetre Radiometer (SMR), a limb‐sounding satellite sensor launched in February 2001. The observations of the chemically passive tracer N 2 O show a subsidence of lower stratospheric air masses inside the Arctic vortex in the range of 3–5 km, or 60–100 K in terms of potential temperature, for the period November 2002 to March 2003. Activated chlorine in the form of ClO was observed inside the vortex from the beginning of December until mid‐February. The accumulated chemical ozone loss over this period, derived from the correlation of ozone with N 2 O, is estimated to be 28 ± 9% on the 50 ppbv level of N 2 O, i.e., for lower stratospheric air masses subsiding from ∼23 down to 19 km, the lower limit of the Odin/SMR ozone measurement in the 501.8 GHz band.