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Fig. 3 | Earth, Planets and Space

Fig. 3

From: Observations of stratospheric and mesospheric O3 with a millimeter-wave radiometer at Rikubetsu, Japan

Fig. 3

Time series of scaling factors for correcting spectral intensity. The scaling factors are derived from the ozonesonde profiles up to the balloon burst height (at least 26 km) and MLS monthly mean climatology above the burst height (red circles). Black circles show alternate scaling factors obtained for each spectrum by using the MLS climatology over all altitude ranges, instead of the ozonesonde profile. Green dash lines indicate the times of the change in the instrumentation described in Table 1

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