Comparison of14CO2, CO, and SF6as tracers for recently added fossil fuel CO2in the atmosphere and implications for biological CO2exchange-Reference-Cited by-同舟云学术

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Comparison of14CO2, CO, and SF6as tracers for recently added fossil fuel CO2in the atmosphere and implications for biological CO2exchange

Published:2006-01-14 Issue:1 Volume:33 Page:n/a-n/a
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Turnbull J. C.¹,Miller J. B.²³,Lehman S. J.¹,Tans P. P.²,Sparks R. J.⁴,Southon J.⁵

Affiliation:

1. Institute of Arctic and Alpine Research; University of Colorado; Boulder Colorado USA

2. Climate Monitoring and Diagnostics Laboratory; NOAA; Boulder Colorado USA

3. Cooperative Institute for Research in Environmental Sciences; University of Colorado; Boulder Colorado USA

4. Rafter Radiocarbon Laboratory; Lower Hutt New Zealand

5. Department of Earth System Science; University of California; Irvine California USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference19 articles.

1. Determination of the isotopic (13C/12C) discrimination by terrestrial biology from a global network of observations;Bakwin;Global Biogeochem. Cycles,1998

2. Regional carbon dioxide fluxes from mixing ratio data;Bakwin;Tellus, Ser. B,2004

3. Inverse modeling of the global CO cycle: 1. Inversion of CO mixing ratios;Bergamaschi;J. Geophys. Res.,2000

4. Tropospheric SF6: Observed latitudinal distribution and trends, derived emissions and interhemispheric exchange time;Geller;Geophys. Res. Lett.,1997

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