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

The lifetimes of CFC-11 and CFC-12 have been evaluated using global observations of their stratospheric distributions from satellite-based instruments over the time period from 1992 to 2010. The chlorofluorocarbon (CFC) datasets are from the Cryogen Limb Array Etalon Spectrometer (CLAES), the Cryoge...

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Main Authors: K. Minschwaner, L. Hoffmann, A. Brown, M. Riese, R. Müller, P. F. Bernath
Format: Article
Language:English
Published: Copernicus Publications 2013-04-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/13/4253/2013/acp-13-4253-2013.pdf
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spelling doaj-c8ab8a68cf0343318dc843a020371ed42020-11-24T23:06:10ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242013-04-011384253426310.5194/acp-13-4253-2013Stratospheric loss and atmospheric lifetimes of CFC-11 and CFC-12 derived from satellite observationsK. MinschwanerL. HoffmannA. BrownM. RieseR. MüllerP. F. BernathThe lifetimes of CFC-11 and CFC-12 have been evaluated using global observations of their stratospheric distributions from satellite-based instruments over the time period from 1992 to 2010. The chlorofluorocarbon (CFC) datasets 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 44.7 (36–58) yr for CFC-11 and 106.6 (90–130) yr for CFC-12, which are in good agreement with the most recent WMO ozone assessment. There are two major sources of error in calculating lifetimes using this method. The first important error arises from uncertainties in tropical stratospheric observations, particularly for CFC-11. Another large contribution to the error is due to 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.http://www.atmos-chem-phys.net/13/4253/2013/acp-13-4253-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author K. Minschwaner
L. Hoffmann
A. Brown
M. Riese
R. Müller
P. F. Bernath
spellingShingle K. Minschwaner
L. Hoffmann
A. Brown
M. Riese
R. Müller
P. F. Bernath
Stratospheric loss and atmospheric lifetimes of CFC-11 and CFC-12 derived from satellite observations
Atmospheric Chemistry and Physics
author_facet K. Minschwaner
L. Hoffmann
A. Brown
M. Riese
R. Müller
P. F. Bernath
author_sort K. Minschwaner
title Stratospheric loss and atmospheric lifetimes of CFC-11 and CFC-12 derived from satellite observations
title_short Stratospheric loss and atmospheric lifetimes of CFC-11 and CFC-12 derived from satellite observations
title_full Stratospheric loss and atmospheric lifetimes of CFC-11 and CFC-12 derived from satellite observations
title_fullStr Stratospheric loss and atmospheric lifetimes of CFC-11 and CFC-12 derived from satellite observations
title_full_unstemmed Stratospheric loss and atmospheric lifetimes of CFC-11 and CFC-12 derived from satellite observations
title_sort stratospheric loss and atmospheric lifetimes of cfc-11 and cfc-12 derived from satellite observations
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2013-04-01
description The lifetimes of CFC-11 and CFC-12 have been evaluated using global observations of their stratospheric distributions from satellite-based instruments over the time period from 1992 to 2010. The chlorofluorocarbon (CFC) datasets 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 44.7 (36–58) yr for CFC-11 and 106.6 (90–130) yr for CFC-12, which are in good agreement with the most recent WMO ozone assessment. There are two major sources of error in calculating lifetimes using this method. The first important error arises from uncertainties in tropical stratospheric observations, particularly for CFC-11. Another large contribution to the error is due to 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.
url http://www.atmos-chem-phys.net/13/4253/2013/acp-13-4253-2013.pdf
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