Inversion using IMAGES model

Introduction Conclusions References Tables Figures Back Close Abstract Introduction Conclusions References Tables Figures Back Close Abstract We use ground-based observations of CO mixing ratios and vertical column abundances together with tropospheric NO 2 columns from the GOME satellite instrument as constraints for improving the global annual emission estimates of CO and NO x for the year 1997. The agreement between concentrations calculated by the global 3-5 dimensional CTM IMAGES and the observations is optimized using the adjoint modelling technique, which allows to invert for CO and NO x fluxes simultaneously, taking their chemical interactions into account. Our analysis quantifies a total of 39 flux parameters, comprising anthropogenic and biomass burning sources over large continental regions, soil and lightning emissions of NO x , biogenic emissions of CO and 10 non-methane hydrocarbons, as well as the deposition velocities of both CO and NO x. Comparison between observed, prior and optimized CO mixing ratios at NOAA/CMDL sites shows that the inversion performs well at the northern mid-and high latitudes, and that it is less efficient in the Southern Hemisphere, as expected due to the scarsity of measurements over this part of the globe. The inversion, moreover, brings the model 15 much closer to the measured NO 2 columns over all regions. Sensitivity tests show that anthropogenic sources exhibit weak sensitivity to changes of the a priori errors associated to the bottom-up inventory, whereas biomass burning sources are subject to a strong variability. Our best estimate for the 1997 global top-down CO source amounts to 2760 Tg CO. Anthropogenic emissions increase by 28%, in agreement with previous 20 inverse modelling studies, suggesting that the present bottom-up inventories underestimate the anthropogenic CO emissions in the Northern Hemisphere. The magnitude of the optimized NO x global source decreases by 14% with respect to the prior, and amounts to 42.1 Tg N, out of which 22.8 Tg N are due to anthropogenic sources. The NO x emissions increase over Tropical regions, whereas they decrease over Europe 25 and Asia. Our inversion results have been evaluated against independent observations from aircraft campaigns. This comparison shows that the optimization of CO emissions constrained by both CO and NO 2 observations leads to a better agreement 7986 Abstract Introduction Conclusions References Tables Figures Back Close Full Screen / Esc Print Version Interactive Discussion EGU between modelled and observed values, especially in the Tropics and the Southern Hemisphere, compared to …