The absorption of nearly half of all anthropogenic carbon dioxide (CO2) emissions by terrestrial and marine ecosystems has played a critical role in mitigating climate change. However, a persistent lack of understanding of these uptake processes impedes attribution, and thereby introduces large uncertainties into projections of the trajectory of carbon and climate in coming decades. A better understanding and quantification of the seasonal and interannual variability of carbon flux between the atmosphere and ocean and terrestrial biospheres is critically needed to improve predictions from Earth system models. We propose to bring together a diverse suite of remote sensing observations, mechanistic models, and NASA's Goddard Earth Observing S...
Atmospheric carbon dioxide (CO2) accounts for the largest radiative forcing among anthropogenic gree...
In order to devise strategies to reduce atmospheric CO2 concentrations and predict their future traj...
With representation of the global carbon cycle becoming increasingly complex in climate models, it i...
Reliable projections of climate change will require terrestrial biosphere models (TBMs) that produce...
Seasonal forecasts made by coupled atmosphere-ocean general circulation models (GCMs) are increasing...
There is considerable uncertainty as to whether interannual variability in climate and terrestrial e...
We evaluate the GEOS-Chem atmospheric transport model (v8-02-01) of CO2 over 2003–2006, driven by GE...
Seasonal and interannual variability in atmospheric carbon dioxide (CO2) concentrations was simulate...
Results of an intercomparison among terrestrial biogeochemical models (TBMs) are reported, in which ...
Model results will be reviewed to assess different methods for bounding the terrestrial role in the ...
Results of an intercomparison among terrestrial biogeochemical models (TBMs) are reported, in which ...
International audienceYear-to-year variability in CO2 fluxes can yield insight into climate-carbon c...
Column CO2 observations from current and future remote sensing missions represent a major advancemen...
[EN] Quantifying ecosystem carbon fluxes and stocks is essential for better understanding the global...
To better understand the role of terrestrial ecosystems in the global carbon cycle and their feedbac...
Atmospheric carbon dioxide (CO2) accounts for the largest radiative forcing among anthropogenic gree...
In order to devise strategies to reduce atmospheric CO2 concentrations and predict their future traj...
With representation of the global carbon cycle becoming increasingly complex in climate models, it i...
Reliable projections of climate change will require terrestrial biosphere models (TBMs) that produce...
Seasonal forecasts made by coupled atmosphere-ocean general circulation models (GCMs) are increasing...
There is considerable uncertainty as to whether interannual variability in climate and terrestrial e...
We evaluate the GEOS-Chem atmospheric transport model (v8-02-01) of CO2 over 2003–2006, driven by GE...
Seasonal and interannual variability in atmospheric carbon dioxide (CO2) concentrations was simulate...
Results of an intercomparison among terrestrial biogeochemical models (TBMs) are reported, in which ...
Model results will be reviewed to assess different methods for bounding the terrestrial role in the ...
Results of an intercomparison among terrestrial biogeochemical models (TBMs) are reported, in which ...
International audienceYear-to-year variability in CO2 fluxes can yield insight into climate-carbon c...
Column CO2 observations from current and future remote sensing missions represent a major advancemen...
[EN] Quantifying ecosystem carbon fluxes and stocks is essential for better understanding the global...
To better understand the role of terrestrial ecosystems in the global carbon cycle and their feedbac...
Atmospheric carbon dioxide (CO2) accounts for the largest radiative forcing among anthropogenic gree...
In order to devise strategies to reduce atmospheric CO2 concentrations and predict their future traj...
With representation of the global carbon cycle becoming increasingly complex in climate models, it i...