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CERFACS CERFACS Scientific Activity Report Jan. 2010 – Dec. 2011

CERFACS CERFACS Scientific Activity Report Jan. 2010 – Dec. 2011

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DATA ASSIMILATION FOR ATMOSPHERIC CHEMISTRY<br />

In the regional version of MOCAGE-Valentina, we have performed several experiments assimilating surface<br />

ozone measurement. The experiments also differ by the choice of the BECM configuration, in which<br />

the correlations and standard deviations matrices come from the ensemble-based diagnostics or from a<br />

posteriori diagnostics. All the analyses from these experiments are very well correlated to the observations,<br />

what assimilated or validation stations. Comparisons of the analyses with the validation stations show that<br />

the use of a BECM with time-dependent length-scales gives the largest correlation. All the analyses have a<br />

better correlation with the observations than the direct MOCAGE simulation, but the differences between<br />

them are small and we cannot conclude which BECM formulation is the most appropriate to the ozone<br />

simulation over Europe. The impact of the BECM formulation has been also difficult to evaluate because<br />

the model MOCAGE shows systematic bias in situation with low ozone concentration. So the impact of the<br />

analysis process is mostly to remove this bias.<br />

3.4 Development of linear chemistry schemes (S. Massart,<br />

D. Cariolle J. Flemming)<br />

During those past years a linearised ozone photochemical scheme has been developed for use within<br />

GCMs and CTMs. This scheme is widely used for climate simulations and data assimilation studies. The<br />

computational cost of this scheme is very low since it only requires an additional continuity equation to<br />

be solved in the large scale models. We had therefore extended the methodology to treat other chemical<br />

species, in particular a linearised scheme has been derived for CO and was implement in MOCAGE<br />

[DA3, DA12, DA4]. CO is one of the most important tropospheric trace gases. In particular because it<br />

affects the concentrations of the OH radical. Moreover the main sources of CO are incomplete fossil fuel<br />

and biomass burning, which lead to enhanced surface concentrations. And with a lifetime of a few months<br />

CO can serve as a tracer for regional and inter-continental transport of polluted air.<br />

Within MACC a major development effort of the Global Reactive Gases sub-project is the on-line<br />

integration of the chemistry in the IFS (known as C-IFS). C-IFS aims at a modular implementation of the<br />

chemical scheme used in several global CTMs including MOCAGE. To complement the complex schemes,<br />

linear scheme are explored in C-IFS for their potential in computational demanding application such as<br />

high resolution simulations and data assimilation. So, in parallel with the comprehensive detailed chemical<br />

schemes, we implemented in C-IFS the linearised parameterisation for CO.<br />

(a) GEMS reanalysis<br />

(b) High resolution simulation<br />

FIG. 3.4: CO concentration (in ppbv) at 500 hPa for the 19 th <strong>Jan</strong>uary 2008.<br />

82 <strong>Jan</strong>. <strong>2010</strong> – <strong>Dec</strong>. <strong>2011</strong>

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