Extreme <sup>13</sup>C depletion of CCl<sub>2</sub>F<sub>2</sub> in firn air samples from NEEM, Greenland

A series of 12 high volume air samples collected from the S2 firn core during the North Greenland Eemian Ice Drilling (NEEM) 2009 campaign have been measured for mixing ratio and stable carbon isotope composition of the chlorofluorocarbon CFC-12 (CCl<sub>2</sub>F<sub>2</sub>)...

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Main Authors: T. Blunier, V. Petrenko, D. Etheridge, E. Witrant, J. Kaiser, R. Schneider, P. Martinerie, R. Holzinger, A. Zuiderweg, T. Röckmann
Format: Article
Language:English
Published: Copernicus Publications 2013-01-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/13/599/2013/acp-13-599-2013.pdf
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spelling doaj-fadfac95c198445e9110d1137e26156f2020-11-25T00:18:22ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242013-01-0113259960910.5194/acp-13-599-2013Extreme <sup>13</sup>C depletion of CCl<sub>2</sub>F<sub>2</sub> in firn air samples from NEEM, GreenlandT. BlunierV. PetrenkoD. EtheridgeE. WitrantJ. KaiserR. SchneiderP. MartinerieR. HolzingerA. ZuiderwegT. RöckmannA series of 12 high volume air samples collected from the S2 firn core during the North Greenland Eemian Ice Drilling (NEEM) 2009 campaign have been measured for mixing ratio and stable carbon isotope composition of the chlorofluorocarbon CFC-12 (CCl<sub>2</sub>F<sub>2</sub>). While the mixing ratio measurements compare favorably to other firn air studies, the isotope results show extreme <sup>13</sup>C depletion at the deepest measurable depth (65 m), to values lower than &delta;<sup>13</sup>C = −80&permil; vs. VPDB (the international stable carbon isotope scale), compared to present day surface tropospheric measurements near −40&permil;. Firn air modeling was used to interpret these measurements. Reconstructed atmospheric time series indicate even larger depletions (to −120&permil;) near 1950 AD, with subsequent rapid enrichment of the atmospheric reservoir of the compound to the present day value. Mass-balance calculations show that this change is likely to have been caused by a large change in the isotopic composition of anthropogenic CFC-12 emissions, probably due to technological advances in the CFC production process over the last 80 yr, though direct evidence is lacking.http://www.atmos-chem-phys.net/13/599/2013/acp-13-599-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author T. Blunier
V. Petrenko
D. Etheridge
E. Witrant
J. Kaiser
R. Schneider
P. Martinerie
R. Holzinger
A. Zuiderweg
T. Röckmann
spellingShingle T. Blunier
V. Petrenko
D. Etheridge
E. Witrant
J. Kaiser
R. Schneider
P. Martinerie
R. Holzinger
A. Zuiderweg
T. Röckmann
Extreme <sup>13</sup>C depletion of CCl<sub>2</sub>F<sub>2</sub> in firn air samples from NEEM, Greenland
Atmospheric Chemistry and Physics
author_facet T. Blunier
V. Petrenko
D. Etheridge
E. Witrant
J. Kaiser
R. Schneider
P. Martinerie
R. Holzinger
A. Zuiderweg
T. Röckmann
author_sort T. Blunier
title Extreme <sup>13</sup>C depletion of CCl<sub>2</sub>F<sub>2</sub> in firn air samples from NEEM, Greenland
title_short Extreme <sup>13</sup>C depletion of CCl<sub>2</sub>F<sub>2</sub> in firn air samples from NEEM, Greenland
title_full Extreme <sup>13</sup>C depletion of CCl<sub>2</sub>F<sub>2</sub> in firn air samples from NEEM, Greenland
title_fullStr Extreme <sup>13</sup>C depletion of CCl<sub>2</sub>F<sub>2</sub> in firn air samples from NEEM, Greenland
title_full_unstemmed Extreme <sup>13</sup>C depletion of CCl<sub>2</sub>F<sub>2</sub> in firn air samples from NEEM, Greenland
title_sort extreme <sup>13</sup>c depletion of ccl<sub>2</sub>f<sub>2</sub> in firn air samples from neem, greenland
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2013-01-01
description A series of 12 high volume air samples collected from the S2 firn core during the North Greenland Eemian Ice Drilling (NEEM) 2009 campaign have been measured for mixing ratio and stable carbon isotope composition of the chlorofluorocarbon CFC-12 (CCl<sub>2</sub>F<sub>2</sub>). While the mixing ratio measurements compare favorably to other firn air studies, the isotope results show extreme <sup>13</sup>C depletion at the deepest measurable depth (65 m), to values lower than &delta;<sup>13</sup>C = −80&permil; vs. VPDB (the international stable carbon isotope scale), compared to present day surface tropospheric measurements near −40&permil;. Firn air modeling was used to interpret these measurements. Reconstructed atmospheric time series indicate even larger depletions (to −120&permil;) near 1950 AD, with subsequent rapid enrichment of the atmospheric reservoir of the compound to the present day value. Mass-balance calculations show that this change is likely to have been caused by a large change in the isotopic composition of anthropogenic CFC-12 emissions, probably due to technological advances in the CFC production process over the last 80 yr, though direct evidence is lacking.
url http://www.atmos-chem-phys.net/13/599/2013/acp-13-599-2013.pdf
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