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Temporal variability of atmospheric oxygen from both continuous measurements and a flask sampling network: Tools for studying the global carbon cycle

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The article was published on 2001-07-01 and is currently open access. It has received 61 citations till now. The article focuses on the topics: Sampling (statistics) & Carbon cycle.

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Book Chapter

The Carbon Cycle and Atmospheric Carbon Dioxide

TL;DR: Contributing Authors D.R.A. Archer, M.M.P. Keeling, D.D.F. Weirig, T. Whorf, A.C. Sitch, R.J. Rayner, S.Q. Tans, H. Yool.
Journal ArticleDOI

Interannual growth rate variations of atmospheric CO2 and its δ13C, H2, CH4, and CO between 1992 and 1999 linked to biomass burning

TL;DR: In this paper, a major fraction of the variability is consistent with two emission pulses coinciding with large biomass burning events in tropical and boreal regions, and observations of unusually high levels of combustion products in the overlying troposphere at these times.
Journal ArticleDOI

The change in oceanic O2 inventory associated with recent global warming

TL;DR: An independent argument is presented here in support of this prediction based on observational evidence of the ocean's biogeochemical response to natural warming, indicating that most of the O2 exchange is biologically mediated through links between heating and stratification.
Journal ArticleDOI

Global oceanic and land biotic carbon sinks from the Scripps atmospheric oxygen flask sampling network

TL;DR: In this paper, a formal framework is described for making optimal use of these data to estimate global oceanic and land biotic carbon sinks for the period 1989-2003 from the Scripps Institution of Oceanography global flask sampling network.
Journal ArticleDOI

Maximum impacts of future reforestation or deforestation on atmospheric CO2

TL;DR: In this paper, the authors make simple but robust calculations of the maximum impact of land-use changes on CO2 in the atmosphere over the next century and show that if all the carbon so far released by landuse changes could be restored to the terrestrial biosphere, atmospheric CO2 concentration at the end of the century would be about 40-70 ppm less than it would be if no such intervention had occurred.
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