Abstract

This paper describes the validation of ozone data from the Upper Atmosphere Research Satellite (UARS) Microwave Limb Sounder (MLS). The MLS ozone retrievals are obtained from the calibrated microwave radiances (emission spectra) in two separate bands, at frequencies near 205 and 183 GHz. Analyses described here focus on the MLS Version 3 data (the first set of files made publicly available). We describe results of simulations performed to assess the quality of the retrieval algorithms, in terms of both mixing ratio and radiance closure. From actual MLS observations, the 205‐GHz ozone retrievals give better closure (smaller radiance residuals) than that from the 183‐GHz measurements and should be considered more accurate from the calibration aspects. However, the 183‐GHz data are less noise limited in the mesosphere and can provide the most useful scientific results in that region. We compare the retrieved 205‐GHz ozone profiles in the middle‐to lower stratosphere to ozonesonde measurements at a wide range of latitudes and seasons. Ground‐based lidar data from Table Mountain, California, provide a good reference for comparisons at higher altitudes. Based on these analyses, comparisons with balloon‐borne measurements and others, as well as a detailed budget of estimated uncertainties, MLS results appear to be generally of high quality, with some biases worth mentioning. Results for the lowermost stratosphere (∼50 to 100 hPa) are still in need of improvement. A set of estimated precision and accuracy values is derived for the MLS ozone data sets. We also comment on recent updates in the retrieval algorithms and their impact on ozone values.

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