Abstract

The Observatoire de Haute Provence (OHP) weekly Electrochemical Concentration Cell (ECC) ozonesonde data have been homogenized for the time period 1991–2020 according to the recommendations of the Ozonesonde Data Quality Assessment (O3S-DQA) panel. The assessment of the ECC homogenization benefit has been carried out using comparisons with ground based instruments also measuring ozone at the same station (lidar, surface measurements) and with collocated satellite observations of the O3 vertical profile by Microwave Limb Sounder (MLS). The major differences between uncorrected and homogenized ECC are related to a change of ozonesonde type in 1997, removal of the pressure dependency of the ECC background current and correction of internal ozonesonde temperature. The 3–4 ppbv positive bias between ECC and lidar in the troposphere is corrected with the homogenization. The ECC 30-years trends of the seasonally adjusted ozone concentrations are also significantly improved both in the troposphere and the stratosphere when the ECC concentrations are homogenized, as shown by the ECC/lidar or ECC/surface ozone trend comparisons. A −0.29 % per year negative trend of the normalization factor (NT) calculated using independent measurements of the total ozone column (TOC) at OHP disappears after homogenization of the ECC. There is however a remaining −5 % negative bias in the TOC which is likely related to an underestimate of the ECC concentrations in the stratosphere above 50 hPa as shown by direct comparison with the OHP lidar and MLS. The reason for this bias is still unclear, but a possible explanation might be related to freezing or evaporation of the sonde solution in the stratosphere. Both the comparisons with lidar and satellite observations suggest that homogenization increases the negative bias of the ECC up to 10 % above 28 km.

Highlights

  • Stratospheric ozone recovery is expected due to a decrease of ozone depleting substances

  • The uncorrected normalization factor (NT) time evolution shows that the dispersion of points is greater before the switch to MODEM ozonesonde in 2007, but more concerning is the significant negative trend of -0.29±0.04% per year which is as large as reported trends in the troposphere (Gaudel et al, 2018)

  • The average normalization factor for the whole date record is not equal to 1 but shows a likely -5% bias Electrochemical Concentration Cell (ECC) total ozone column (TOC) compared to the Observatoire de Haute Provence (OHP) spectrophotometer

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Summary

Introduction

Stratospheric ozone recovery is expected due to a decrease of ozone depleting substances. 100 3 Data and homogenization assessment In this work, the benefit from homogenization of the ECC ozonesonde timeseries is assessed using comparison of homogenized and non homogenized ECC ozone concentrations with other ozone measurements carried out at OHP First these comparisons can be done as a function of altitude using either Ultraviolet DIfferential Absorption Lidar (UV-DIAL) or Microwave Limb Sounder (MLS) satellite observations in the stratosphere (Froidevaux et al, 2008). The corresponding ECC sounding TOC used for the satellite comparison, is calculated using the integration of the ozone concentrations up to 10 hPa and the McPeters and Labow (2012) climatology above 10 hPa. Thirdly the benefit of homogenization on long term ozone trends for several altitude ranges in the troposphere and the stratosphere, has been studied using all the lidar and ECC measurements made at OHP. A significant difference between the two surface concentration trends will point towards a strong sensitivity of the trend sign to the limited number of observations by the ECC

Normalization Factor Trend
Nighttime Ozonesonde/Lidar comparison
Comparison Ozonesonde/Satellite
Conclusions
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