Constraining global air‐sea gas exchange for CO2 with recent bomb 14C measurements

By Colm Sweeney, Emanuel Gloor, A. Jacobson, R. Key, G. McKinley, J. Sarmiento, R. Wanninkhof. 2007

547 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/84eca6fccffd887a8b4308e3f547e4cccb3cc825

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In Global and Planetary Change

1. Peter J. Rayner
2. F. Joos
3. Philippe Ciais
4. John B. Miller
5. R. Roth
6. Frédéric Chevallier

In Oceanography

1. F. Joos
2. R. Roth
3. Peter J. Rayner

Citations in the corpus

• A History of Solar Activity over Millennia (2008, unknown): “On one hand, such sources of momentary spot injections of radioactive tracers (including (14)C) provide a good opportunity to verify and calibrate the exchange parameters for different carbon -cycle reservoirs and circulation models (e.g., Bard et al., 1987; Sweeney et al., 2007).”
• Observations and modelling of the global distribution and long-term trend of atmospheric 14CO2 (2010, background): “…specific aspects of the global carbon cycle, such as studies on air–sea gas exchange (Wanninkhof, 1992; Krakauer et al., 2006; Naegler et al., 2006; Sweeney et al., 2007; Müller et al., 2008; Naegler, 2009), internal mixing of the world oceans (Maier-Reimer and Hasselmann, 1987; Duffy et al.,…”
• A reconstruction of radiocarbon production and total solar irradiance from the Holocene 14 C and CO 2 records: implications of data and model uncertainties (2013, background): “14C permits the quantification of the overturning timescales within the ocean (e.g.Müller et al., 2006) and of the magnitude of the air–sea carbon exchange rate (e.g.Naegler and Levin, 2006; Sweeney et al., 2007; Müller et al., 2008).”
• On the use of 14CO2 as a tracer for fossil fuel CO2: Quantifying uncertainties using an atmospheric transport model (2009, background): “The rate of uptake of excess 14C has been widely used to examine carbon exchange between the atmosphere and oceans [e.g., Müller et al., 2008; Sweeney et al., 2007; Krakauer et al., 2006; Naegler et al., 2006; Hesshaimer et al., 1994; Broecker et al., 1985] and biosphere [e.g., Hahn and Buchmann,…”