Calibration and validation of carbon cycle models is mainly based on isotope data of the steady state of the system as well as its responses to natural and anthropogenic disturbances. The progress in the use of carbon isotopes is reviewed. The discussion covers the following phenomena: - Response of the system to the anthropogenic CO2 input: rise of atmospheric CO2, dilution of the atmospheric 14C concentration - Prenuclear 14C distribution in the ocean - 14C rise in atmosphere and ocean due to bomb produced 14C - Modulation of natural 14C production and its atmospheric response, as reflected in 14C/C ratios recorded in tree-rings - Past changes of the atmospheric CO2 concentration inferred from ice core studies. The informat...
A box-diffusion model for the carbon cycle is used to estimate the magnitude of 14C variations cause...
The recent proposals to estimate the oceanic uptake of CO_2 by monitoring the oceanic change in &quo...
International audienceThis chapter uses the mass-conservation equations for CO2 and its isotopomers ...
The isotopic composition of carbon (Δ14C and δ13C) in atmospheric CO2 and in oceanic and terrestria...
The isotopic composition of carbon (14°C and 13°C) in atmospheric CO2 and in oceanic and terrestrial...
In this "Grand Challenges" paper, we review how the carbon isotopic composition of atmospheric CO2 h...
The long-term variability in the terrestrial and oceanic uptake of anthropogenic carbon is investiga...
Carbon isotopes in the ocean are frequently used as paleoclimate proxies and as present-day geochemi...
A box-diffusion model for the carbon cycle is used to estimate the magnitude of 14C variations cause...
The atmospheric carbon dioxide concentration plays a crucial role in the radiative balance and as su...
The recent proposals to estimate the oceanic uptake of CO2 by monitoring the oceanic change in 13C/1...
Understanding how the Meridional Overturning Circulation (MOC) might change in response to anthropog...
The atmospheric carbon dioxide concentration plays a crucial role in the radiative balance and as su...
Stable isotopes of atmospheric carbon dioxide (CO2) contain a wealth of information regarding biosph...
A summary is given of recent results and unsolved problems regarding the carbon cycle. There is a la...
A box-diffusion model for the carbon cycle is used to estimate the magnitude of 14C variations cause...
The recent proposals to estimate the oceanic uptake of CO_2 by monitoring the oceanic change in &quo...
International audienceThis chapter uses the mass-conservation equations for CO2 and its isotopomers ...
The isotopic composition of carbon (Δ14C and δ13C) in atmospheric CO2 and in oceanic and terrestria...
The isotopic composition of carbon (14°C and 13°C) in atmospheric CO2 and in oceanic and terrestrial...
In this "Grand Challenges" paper, we review how the carbon isotopic composition of atmospheric CO2 h...
The long-term variability in the terrestrial and oceanic uptake of anthropogenic carbon is investiga...
Carbon isotopes in the ocean are frequently used as paleoclimate proxies and as present-day geochemi...
A box-diffusion model for the carbon cycle is used to estimate the magnitude of 14C variations cause...
The atmospheric carbon dioxide concentration plays a crucial role in the radiative balance and as su...
The recent proposals to estimate the oceanic uptake of CO2 by monitoring the oceanic change in 13C/1...
Understanding how the Meridional Overturning Circulation (MOC) might change in response to anthropog...
The atmospheric carbon dioxide concentration plays a crucial role in the radiative balance and as su...
Stable isotopes of atmospheric carbon dioxide (CO2) contain a wealth of information regarding biosph...
A summary is given of recent results and unsolved problems regarding the carbon cycle. There is a la...
A box-diffusion model for the carbon cycle is used to estimate the magnitude of 14C variations cause...
The recent proposals to estimate the oceanic uptake of CO_2 by monitoring the oceanic change in &quo...
International audienceThis chapter uses the mass-conservation equations for CO2 and its isotopomers ...