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Simultaneous measurements of OClO, NO<sub>2</sub> and O<sub>3</sub> in the Arctic polar vortex by the GOMOS instrument

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Fig. 1. On the left: vertical profiles of NO 2 slant column densities for August 2003 in the [60 ◦ – 65 ◦ S] latitudinal band
Fig. 2. Potential vorticity map calculated by the MIMOSA high-resolution advection model at 12:00 UT on 10 January 2008 at 675 K (about 27 km)
Fig. 3. Histogram of transmittances at 30 km and at 386 nm from the GOMOS Sirius occulta- occulta-tions in January 2008 in the 70–75 ◦ N latitudinal range.
Fig. 4. OClO slant column densities as a function of longitude with the spectral inversion error bars for January 2008 in the Arctic polar region
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