Growth rates of stratospheric HCFC-22

The Michelson Interferometer for Passive Atmospheric Sounding onboard ENVISAT (MIPAS-E) offers the opportunity to detect and spectrally resolve many atmospheric minor constituents affecting atmospheric chemistry. In this paper, we describe an algorithm produced to retrieve HCFC–22 prof...

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Main Authors: D. P. Moore, J. J. Remedios
Format: Article
Language:English
Published: Copernicus Publications 2008-01-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/8/73/2008/acp-8-73-2008.pdf
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author D. P. Moore
J. J. Remedios
author_facet D. P. Moore
J. J. Remedios
author_sort D. P. Moore
collection DOAJ
description The Michelson Interferometer for Passive Atmospheric Sounding onboard ENVISAT (MIPAS-E) offers the opportunity to detect and spectrally resolve many atmospheric minor constituents affecting atmospheric chemistry. In this paper, we describe an algorithm produced to retrieve HCFC–22 profiles from MIPAS-E measurements made in 2003 and present results from this scheme between 300 and 50 mb. By comparison with ATMOS (AT–3) version 3 data, we find a mean Northern Hemisphere mid-latitude (20–50° N) HCFC–22 growth rate between 1994 and 2003 of 5.4±0.7 pptv/yr in the lower stratosphere (LS) and a mean LS Southern Hemisphere growth rate (60–80° S) of 6.0±0.7 pptv/yr in the same period. We test the feasibility of using a global data set to estimate the chemical lifetime of HCFC–22 in the LS and we derive this for two regions: 20–50° N (246±38 years) and 60–80° S (274±34 years). From these data we note a global LS lifetime of 260±25 years, significantly longer than previous estimates.
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spelling doaj.art-ef7e553335ef453988c692f979c9a9292022-12-22T02:47:15ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242008-01-01817382Growth rates of stratospheric HCFC-22D. P. MooreJ. J. RemediosThe Michelson Interferometer for Passive Atmospheric Sounding onboard ENVISAT (MIPAS-E) offers the opportunity to detect and spectrally resolve many atmospheric minor constituents affecting atmospheric chemistry. In this paper, we describe an algorithm produced to retrieve HCFC–22 profiles from MIPAS-E measurements made in 2003 and present results from this scheme between 300 and 50 mb. By comparison with ATMOS (AT–3) version 3 data, we find a mean Northern Hemisphere mid-latitude (20–50° N) HCFC–22 growth rate between 1994 and 2003 of 5.4±0.7 pptv/yr in the lower stratosphere (LS) and a mean LS Southern Hemisphere growth rate (60–80° S) of 6.0±0.7 pptv/yr in the same period. We test the feasibility of using a global data set to estimate the chemical lifetime of HCFC–22 in the LS and we derive this for two regions: 20–50° N (246±38 years) and 60–80° S (274±34 years). From these data we note a global LS lifetime of 260±25 years, significantly longer than previous estimates.http://www.atmos-chem-phys.net/8/73/2008/acp-8-73-2008.pdf
spellingShingle D. P. Moore
J. J. Remedios
Growth rates of stratospheric HCFC-22
Atmospheric Chemistry and Physics
title Growth rates of stratospheric HCFC-22
title_full Growth rates of stratospheric HCFC-22
title_fullStr Growth rates of stratospheric HCFC-22
title_full_unstemmed Growth rates of stratospheric HCFC-22
title_short Growth rates of stratospheric HCFC-22
title_sort growth rates of stratospheric hcfc 22
url http://www.atmos-chem-phys.net/8/73/2008/acp-8-73-2008.pdf
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