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Ozone structure over the equatorial Andes from balloon-borne observations and zonal connection with two tropical sea level sites

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Abstract

In this paper we present first-time measurements of ozone profiles from a high altitude station in Quito, Ecuador (0.19°S, 78.4°W, and 2391 masl) taken from June 2014 to September 2015. We interpret ozone observations in the troposphere, tropopause, and stratosphere through a zonal comparison with data from stations in the Atlantic and Pacific (Natal and San Cristobal from the SHADOZ network). Tropospheric ozone concentrations above the Andes are lower than ozone over San Cristobal and Natal for similar time periods. Ozone variability and pollution layers are also reduced in the troposphere above the Andes. We explain these differences in terms of reduced contributions from the boundary layer and from horizontal transport. In the tropical tropopause layer, ozone is well-mixed up to near the cold point tropopause level. In this regard, our profiles do not show constraints to deep mixing above 14 km, as has been consistently observed at other tropical stations. Total column ozone and stratospheric column ozone are comparable among the three sites. However, the contribution of tropospheric column ozone to total column ozone is significantly lower above the Andes. Our comparisons provide a connection between observations from tropical stations in equatorial South America separated by the wide continental mass. Identified differences in ozone throughout the atmospheric column demonstrate the global benefit of having an ozone sounding station at the equatorial Andes in support of global monitoring networks.

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Acknowledgments

The EMA station was built by USFQ in 2014. The ozone sounding project at EMA was funded by USFQ through Collaboration Grant CG-2014. Thanks to USFQ authorities for their support throughout the completion of this project. Thanks to Nelson Herrera, Miguel Bravo, and Julieta Juncosa from USFQ for their help with balloon launching logistics and various tasks. Thanks to the SHADOZ program principal investigator (PI) Dr. Anne M. Thompson for making possible long term operations and data availability at SHADOZ stations. Thanks to San Cristobal and Natal PIs (B. Johson and N. Paes Leme) for producing data for the public archive. Thanks to Bryan Johnson and Patrick Cullis from NOAA for their help implementing the ozone sounding capability at EMA USFQ.

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Correspondence to María Cazorla.

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Cazorla, M. Ozone structure over the equatorial Andes from balloon-borne observations and zonal connection with two tropical sea level sites. J Atmos Chem 74, 377–398 (2017). https://doi.org/10.1007/s10874-016-9348-2

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