Besides the flux estimates, global atmospheric fields of CO2 mixing ratios are provided for selected runs. Applications include
The global spatio-temporal CO2 mixing ratio fields have been calculated by forward simulation with the atmospheric tracer transport model TM3 driven with re-analysed meteorological data. Surface CO2 fluxes supplied to the model are the inverse flux estimates, based on atmospheric observations and the same transport model. By construction, therefore, the atmospheric CO2 mixing ratio fields optimally fit the measurements at the set of observation sites used, and provide an interpolation in between.