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Toward a combined SAGE II-HALOE aerosol climatology: an evaluation of HALOE version 19 stratospheric aerosol extinction coefficient observations

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Table 2. HALOE aerosol measurement locations with primary gas species and other absorbers, a indicates that the species is cleared using HALOE derived products (clearing is inferred by the  inclu-sion of their uncertainties in the aerosol uncertainty as no
Fig. 3. This figure shows the median relative uncertainty in the four HALOE aerosol extinction channels between 10 ◦ S and 10 ◦ N and 1996 and 2005 (left) and the median relative standard based on a 3-month running (similar to the analysis shown in Fig
Fig. 4. Median difference between HALOE aerosol extinction coef- coef-ficient at 3.40 and 3.46 µm scaled by a factor of 10 5 and in units of km −1
Fig. 6. These figures show the HALOE 2.45 (a), 3.40 (b) and 5.26 µm (c) to 3.46 µm aerosol extinction ratio relative to the HALOE 3.46 µm to SAGE II 1020-nm aerosol extinction ratio (shown as “+” symbols) computed following the 3-month running medians as s
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