(Q57242402)

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Global and hemispheric CO2 sinks deduced from changes in atmospheric O2 concentration

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Global and hemispheric CO2 sinks deduced from changes in atmospheric O2 concentration (English)

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Martin Heimann

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Ralph Keeling

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Ralph F. Keeling

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Stephen C. Piper

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2

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language of work or name

English

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publication date

May 1996

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Nature

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volume

381

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page(s)

218-221

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6579

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exact match

https://scigraph.springernature.com/pub.10.1038/381218a0

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Observational contrains on the global atmospheric co2 budget.

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Partitioning of ocean and land uptake of CO2as inferred by δ13C measurements from the NOAA Climate Monitoring and Diagnostics Laboratory Global Air Sampling Network

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A Large Northern Hemisphere Terrestrial CO2 Sink Indicated by the 13C/12C Ratio of Atmospheric CO2.

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Atmospheric carbon dioxide and the ocean

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Oceanic Uptake of Fossil Fuel CO2: Carbon-13 Evidence.

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Seasonal and interannual variations in atmospheric oxygen and implications for the global carbon cycle

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Interannual extremes in the rate of rise of atmospheric carbon dioxide since 1980

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Interhemispheric transport of carbon dioxide by ocean circulation

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Carbon Dioxide Transport by Ocean Currents at 25{degrees}N Latitude in the Atlantic Ocean.

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Generalized nonlinear inverse problems solved using the least squares criterion

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Latitudinal gradient of atmospheric CO2 due to seasonal exchange with land biota

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Carbon Dioxide Uptake by an Undisturbed Tropical Rain Forest in Southwest Amazonia, 1992 to 1993

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Changes in oceanic and terrestrial carbon uptake since 1982

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A perturbation simulation of CO2uptake in an ocean general circulation model

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Modelling atmosphere—ocean CO 2 transfer

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Air—sea C02transfer and the carbon budget of the North Atlantic

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Identifiers

DOI

10.1038/381218A0

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1041958523

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(Q57242402)

Global and hemispheric CO2 sinks deduced from changes in atmospheric O2 concentration

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