Inverse modeling of the global CO cycle: 1

By P. Bergamaschi, R. Hein, Martin Heimann, P. Crutzen. 2000

225 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/dd076854f0b7fc6fed36c45862f4d7f3fa6d9ade

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. D. J. Jacob
2. Heinrich Bovensmann
3. Oliver Schneising
4. John P. Burrows
5. Michael Buchwitz
6. Martin Heimann
7. John Gille
8. Paul I. Palmer

In Global and Planetary Change

1. Heinrich Bovensmann
2. Oliver Schneising
3. D. J. Jacob
4. John P. Burrows
5. Michael Buchwitz
6. Paul I. Palmer
7. C. Hewitt
8. C. Heald

Citations in the corpus

• Comparison of Adjoint and Analytical Bayesian Inversion Methods for Constraining Asian Sources of Carbon Monoxide Using Satellite (MOPITT) Measurements of CO Columns (2009, methodology): “It has been applied extensively for example for inverse modeling of CO2 surface fluxes and CO emissions using observations from surface sites [Bousquet et al., 1999; Bergamaschi et al., 2000;Kasibhatla et al., 2002;Pétron et al., 2002] and aircraft [Palmer et al., 2003; Palmer et al., 2006].”
• Atmospheric carbon gases retrieved from SCIAMACHY by WFM-DOAS: version 0.5 CO and CH 4 and impact of calibration improvements on CO 2 retrieval (2006, methodology): “CO plays a central role in tropospheric chemistry (see, e.g., Bergamaschi et al., 2000, and references given therein) as CO is the leading sink of the hydroxyl radical (OH) which itself largely determines the oxidizing capacity of the troposphere and, therefore, its self-cleansing efficiency and…”
• Comparative inverse analysis of satellite (MOPITT) and aircraft (TRACE-P) observations to estimate Asian sources of carbon monoxide (2004, methodology): “[49] Previous inverse modeling studies of CO have employed monthly mean observations from MOPITT [Arellano et al., 2004] or from NOAA/CMDL surface sites [Bergamaschi et al., 2000; Pétron et al., 2002; Kasibhatla et al., 2002].”
• Seasonal NH3 emission estimates for the eastern United States (2003, methodology): “They have been used to estimate global-scale emissions of CFC-11 [Hartley and Prinn, 1993], CO [Bergamaschi et al., 2000], CO 2 [Bousquet et al., 1999], and CH 4 [Houweling et al., 1999; Zhang et al., 1999].”
• Biogenic volatile organic compounds in the Earth system. (2009, background): “Although carbon monoxide (CO) is emitted directly by living, senescing and dead leaves (Tarr et al., 1995), the oxidation of BVOCs also contributes significant amounts of CO to the atmosphere (Hatakeyama et al., 1991; Fehsenfeld et al., 1992; Bergamaschi et al., 2000; Griffin et al., 2007).”