Abstract

To further verify the ozone profile reliability of satellite remote sensing for the ozone valley over the Tibetan Plateau in the core area of the South Asian high in summer, we validate the ozone products from the microwave limb sounder (MLS) onboard the Aura satellite over the Tibetan plateau using electrochemical concentration cell (ECC) ozonesonde data of 2016 for Ngari, Tibet. The MLS version four ozone profiles have lower standard deviation in the middle stratosphere (38–10 hPa), whereas the ozonesonde profiles have lower standard deviation in the upper troposphere and lower stratosphere region (200–83 hPa). There are statistically significant differences between these two datasets in most of the stratosphere (10–83 hPa). The mean value of MLS ozone is about 0.8–1.5 mPa greater than that of ECC ozone, which corresponds to a relative deviation of 59 ± 24% at 83 hPa, 24 ± 13% at 68 hPa, 20 ± 5% at 56 hPa, 14 ± 4% at 46 hPa and 38 hPa, and 9 ± 4% in the layers between 32 and 10 hPa. However, there is no statistically significant difference between the two datasets in the upper troposphere (100–200 hPa).

Highlights

  • The stratospheric ozone layer absorbs solar ultraviolet radiation and heats the atmosphere

  • There is a large depression in total column ozone of ~30 DU relative to the surrounding area in the upper troposphere and lower stratosphere (UTLS) region over the Tibetan Plateau [1,2,3,4,5,6], which is under the influence of the South Asian high in summer

  • Most ozone profile data are derived from satellite remote sensing instruments; for example, the Halogen Occultation Experiment (HALOE) [7], the Stratospheric Aerosol and Gas Experiment (SAGE) [8], and the microwave limb sounder (MLS) [9]

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Summary

Introduction

The stratospheric ozone layer absorbs solar ultraviolet radiation and heats the atmosphere. This has an important impact on the dynamical and thermodynamic structure of the stratosphere. Most ozone profile data are derived from satellite remote sensing instruments; for example, the Halogen Occultation Experiment (HALOE) [7], the Stratospheric Aerosol and Gas Experiment (SAGE) [8], and the microwave limb sounder (MLS) [9]. The remote-sensing algorithm used for ozone profiles shows little difference in zonal distribution, but the actual local dynamic and thermal structures vary widely, resulting in a large deviation in ozone profiles in certain locations.

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