An intercomparison of inverse models for estimating sources and sinks of CO 2 using GOSAT measurements

In December, when model results of S EMEP and S EMEP c can be compared to artefact-free NO − 3 aerosol measurements (ES Table S19, 16 stations, including stations with tempo-.. de

• La définition et la mise en oeuvre du Plan Solaire Togolais, des plans solaires des états membres de l'UEMOA pour les intégrer dans le Plan Solaire UEMOA,

Because the two stress-disturbance mechanisms we considered in our model (erosion and horizontal straining) do not affect vertical gradients of principal stresses, the value of

Our density data analyses (14-17), performed in order to improve the first models which were mainly based on orbital data of satellites with perigee greater than 250 km,

Centré sur l’Afrique occidentale française, l’ouvrage de Jean- Paul Bado traite, à partir de trois endémies (lèpre, trypanosomiase et onchocercose), de la

We show that the effective diffusion tensor obtained by mathematical homogenization theory (see e.g. [2,3]) is a good approximation to the long time apparent diffusion tensor

This fibrous clay presents parallel channels running along the fibres in the c direction (Fig. At room temperature, tunnels are filled with weakly bound zeolitic water, released

This implies that the big flake undergoes a more important uniform tensile strain than the small flake; this can be justi fied by the different orientation of these flakes grown