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Pole-to-pole validation of GOME WFDOAS total ozone with ground-based data, Atmos. Chem. Phys, vol.5, pp.1341-1355, 2005. ,
The Brewer-Dobson circulation and total ozone from seasonal to decadal time scales, Atmos. Chem. Phys, vol.11, pp.221-232, 2011. ,
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Chemical and dynamical contributions to ozone profile trends of the Payerne (Switzerland) balloon soundings, J. Geophys. Res, vol.106, issue.D19, pp.685-707, 2001. ,
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Ground-based instruments at numerous stations around the globe monitor changes in total column and profile ozone amounts at local to regional scales (WMO, SAOZ spectrometers, p.microwave radiometers, 1988. ,
Calisesi et al, 1992. ,
) and aircraft-mounted sensors, situ instruments such as balloon-borne ozonesondes, 1969. ,
The Payerne microwave data changed as a result of improvements in the retrieval method and in the integration of the measurements (private communications with PI Maillard-Barras). Both revised MWR records were used for this Assessment. Over the past few years, the ozonesonde community has put considerable effort into reducing uncertainties in the measurements to 5-10%. Biases between different types of ozonesonde instrumentation have been characterized, correction schemes developed, and the ozone profile records of 30 stations in the NDACC, GAW, and SHADOZ networks reprocessed accordingly, Since the last Assessment, most ground-based data records were merely extended in time, 2015. ,
Further efforts to assess the outcome of this homogenization activity are ongoing. At the time of this Assessment, not all reprocessed sonde data were available, 2018. ,
The profile trends assessed here are based on observations at the sites listed in Table 3A-1, most of which have operated continuously for at least 20 years. Zonally averaged, ground-based data records, one for each measurement technique, were computed from deseasonalized anomaly time series at each site in a given latitude band, LOTUS, 2002. ,
Time series based on these relatively sparse ground-based measurements may not always reproduce monthly zonal fluctuations well, particularly in the tropics and Southern Hemisphere. However, seasonal (and longer) averages can be estimated, The WOUDC ground-based total column dataset is based on available Dobson, 2002. ,
Space-Based Ozone Profiles Space-based observations of stratospheric ozone are performed in nadir-, limb-, or occultation-viewing geometry in different wavelength ranges using different measurement techniques, 2014. ,
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