Assessing the potential long-term increase of oceanic fossil fuel CO₂ uptake due to CO₂-calcification feedback

The two main anthropogenic CO 2 fluxes are emissions from the combustion of fossil fuels and net emissions from land use change, the latter being largely driven by deforestation

We have used the GEOS-Chem CO 2 simulation with CO 2 emissions from global monthly-varying fossil fuel use, shipping, aviation and the chemical production of CO 2 from the oxidation

Model estimated CO 2 time series at two surface stations in the southern extra-tropics, compared to CO 2 measurements taken at those stations.. The “GOSAT” line is from an

To investigate whether changing the gas transfer rate can improve regional model prediction, we compared the results from the model runs with the climatology of Taka- hashi et al.

CO 2 emission (t h −1 ) of Caterpillar bulldozers at various engine load factors was determined using an hourly fuel consumption and conversion factor of CF = 0.00268 for

transport model and a minimum variance Bayesian inverse method was used to estimate annual emission rates using the measurements, with a priori estimates from the Emis- sions

The framework is based on a mass balance ap- proach and given that for Europe most of the components have been independently estimated, di ff erent accounting schemes may be used

Another impact of non-acyl peroxy nitrates is that they are a possible positive inter- ference to in-situ NO 2 measurements in the upper troposphere because the non-acyl peroxy