References

ACPD

Atmospheric Chemistry and Physics Discussions

ACPD

1680-7375

Copernicus GmbH

Göttingen, Germany

10.5194/acpd-12-28733-2012

Stratospheric loss and atmospheric lifetimes of CFC-11 and CFC-12 derived from satellite observations

Minschwaner

¹ Hoffmann

² Brown

³ Riese

⁴ Müller

⁴ Bernath

P. F.

³ ⁵

Department of Physics, New Mexico Institute of Mining and Technology, Socorro, USA

Jülich Supercomputing Centre (JSC), Forschungszentrum Jülich, Germany

Department of Chemistry, University of York, UK

Institute of Energy and Climate Research (IEK-7), Forschungszentrum Jülich, Germany

Department of Chemistry and Biochemistry, Old Dominion University, Norfolk, VA, USA

05 11 2012

12 11 28733 28764

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The lifetimes of CFC-11 and CFC-12 have been evaluated using global observations of their stratospheric distributions from satellite-based instruments between the period 1992 and 2010. The CFC data sets are from the Cryogen Limb Array Etalon Spectrometer (CLAES), the Cryogenic Infrared Spectrometers and Telescopes for the Atmosphere (CRISTA-1 and CRISTA-2), the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS), and the Atmospheric Chemistry Experiment (ACE). Stratospheric loss rates were calculated using an ultraviolet radiative transfer code with updated cross section and solar irradiance data. Mean steady state lifetimes based on these observations are 50.3 ± 16.8 yr for CFC-11 and 106.9 ± 21.7 yr for CFC-12, which are in reasonable agreement with the most recent WMO Ozone Assessment recommendations but are somewhat longer by 12% and 7%, respectively. There are two major sources of error in calculating lifetimes using this method. One error source is due to uncertainties in tropical stratospheric measurements, particularly for CFC-11. Another large contribution to the error arises from uncertainties in the penetration of solar ultraviolet radiation at wavelengths between 185 and 220 nm, primarily in the tropical stratosphere between 20 and 35 km altitude.

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