By Brian J. McPherson, Eric T. Sundquist
Published by way of the yank Geophysical Union as a part of the Geophysical Monograph Series.
For carbon sequestration the problems of tracking, possibility evaluation, and verification of carbon content material and garage efficacy are possibly the main doubtful. but those matters also are the main serious demanding situations dealing with the wider context of carbon sequestration as a way for addressing weather switch. in keeping with those demanding situations, Carbon Sequestration and Its function within the worldwide Carbon Cycle offers present views and study that mix 5 significant components:
- The worldwide carbon cycle and verification and evaluation of world carbon assets and sinks
- Potential capability and temporal/spatial scales of terrestrial, oceanic, and geologic carbon storage
- Assessing hazards and merits linked to terrestrial, oceanic, and geologic carbon storage
- Predicting, tracking, and verifying effectiveness of alternative types of carbon storage
- Suggested new CO2 sequestration learn and administration paradigms for the future.
The quantity is predicated on a Chapman convention and should attract the swiftly starting to be crew of scientists and engineers analyzing equipment for planned carbon sequestration via garage in vegetation, soils, the oceans, and geological repositories.
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Extra resources for Carbon Sequestration and Its Role in the Global Carbon Cycle
1965, p. 127]. This was a clear reference to the Weather Bureau–supported Scripps CO2 program. S. Government” had “specif- ically charged” the Environmental Science Services Administration (ESSA, which housed the Weather Bureau) “with continuing the surveillance of background CO2” (L. Machta, letter to W. Bischof, 23 December 1965). The letter omitted the report’s recommendation concerning the Weather Bureau “and its collaborators,” which had obviously been a reference to CDK and the Scripps CO2 program.
Bolin (1967), The simultaneous use of chemical tracers in oceanic studies. I. General theory of reservoir models, Tellus, 19, 566–581. Keeling, C. , and B. Bolin (1968), The simultaneous use of chemical tracers in oceanic studies. II. A three-reservoir model of the North and South Pacific oceans, Tellus, 20, 17–54. Keeling, C. , R. B. Bacastow, A. E. Bainbridge, C. A. , P. R. Guenther, L. S. Waterman, and J. F. S. Chin (1976a), Atmospheric carbon dioxide variations at Mauna Loa Observatory, Hawaii, Tellus, 28, 538–551.
1029/JZ070i024p06077. Ekdahl, C. , and C. D. Keeling (1973), Atmospheric carbon dioxide and radiocarbon in the natural carbon cycle: I. Quantitative deductions from the records of Mauna Loa Observatory and at the South Pole, in Carbon and the Biosphere, Brookhaven Symp. , vol. 24, edited by G. M. Woodwell and E. V. Pecan, pp. S. At. , Washington, D. C. Farman, J. , B. G. Gardiner, and J. D. 1038/315207a0. Keeling, C. D. (1958). The concentration and isotopic abundances of atmospheric carbon dioxide in rural areas, Geochim.
Carbon Sequestration and Its Role in the Global Carbon Cycle by Brian J. McPherson, Eric T. Sundquist