The O2 Balance of the Atmosphere: A Tool for Studying the Fate of Fossil-Fuel CO2
Abstract
Carbon dioxide is a radiatively active gas whose atmospheric concentration increase is likely to affect Earth's climate. CO2 is added to the atmosphere by biomass burning and the combustion of fossil fuels. Some added CO2 remains in the atmosphere. However, substantial amounts are taken up by the oceans and land biosphere, attenuating the atmospheric increase. Atmospheric O2 measurements provide one constraint for partitioning uptake rates between the ocean and the land biosphere. Here we review studies of atmospheric O2 concentration variations and discuss their implications for CO2 uptake by the ocean and the land biosphere.
- Authors:
-
- Princeton University, Department of Geosciences; ESS-DIVE
- Bowdoin College
- University of California, Scripps Institution of Oceanography
- Publication Date:
- Other Number(s):
- cdiac:O2/N2 data
- Research Org.:
- Environmental System Science Data Infrastructure for a Virtual Ecosystem
- Subject:
- 54 ENVIRONMENTAL SCIENCES; American Samoa: Delta; Baring Head, New Zealand: Delta; CO2; Cape Grim, Tasmania: Delta; Carbon Dioxide; Collection Date; Global; N2; O2; Point Barrow, AK: Delta; Station; Syowa, Antarctica: Delta; carbon; cycle; global carbon cycle
- OSTI Identifier:
- 1464236
- DOI:
- https://doi.org/10.15485/1464236
Citation Formats
Bender, M. L., Battle, M., and Keeling, R. The O2 Balance of the Atmosphere: A Tool for Studying the Fate of Fossil-Fuel CO2. United States: N. p., 1997.
Web. doi:10.15485/1464236.
Bender, M. L., Battle, M., & Keeling, R. The O2 Balance of the Atmosphere: A Tool for Studying the Fate of Fossil-Fuel CO2. United States. doi:https://doi.org/10.15485/1464236
Bender, M. L., Battle, M., and Keeling, R. 1997.
"The O2 Balance of the Atmosphere: A Tool for Studying the Fate of Fossil-Fuel CO2". United States. doi:https://doi.org/10.15485/1464236. https://www.osti.gov/servlets/purl/1464236. Pub date:Wed Dec 31 23:00:00 EST 1997
@article{osti_1464236,
title = {The O2 Balance of the Atmosphere: A Tool for Studying the Fate of Fossil-Fuel CO2},
author = {Bender, M. L. and Battle, M. and Keeling, R.},
abstractNote = {Carbon dioxide is a radiatively active gas whose atmospheric concentration increase is likely to affect Earth's climate. CO2 is added to the atmosphere by biomass burning and the combustion of fossil fuels. Some added CO2 remains in the atmosphere. However, substantial amounts are taken up by the oceans and land biosphere, attenuating the atmospheric increase. Atmospheric O2 measurements provide one constraint for partitioning uptake rates between the ocean and the land biosphere. Here we review studies of atmospheric O2 concentration variations and discuss their implications for CO2 uptake by the ocean and the land biosphere.},
doi = {10.15485/1464236},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Wed Dec 31 23:00:00 EST 1997},
month = {Wed Dec 31 23:00:00 EST 1997}
}
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