Abstract. The overall objective of the present study is to introduce the new ECOCLIMAP-II database for Europe, which is an upgrade for this region of the former initiative, ECOCLIMAP-I, already implemented at global scale. The ECOCLIMAP programme is a dual database at 1 km resolution that includes an ecosystem classification and a coherent set of land surface parameters that are primarily mandatory in meteorological modelling (notably leaf area index and albedo). Hence, the aim of this innovative physiography is to enhance the quality of initialisation and impose some surface attributes within the scope of weather forecasting and climate related studies. The strategy for implementing ECOCLIMAP-II is to depart from prevalent land cover products such as CLC2000 (Corine Land Cover) and GLC2000 (Global Land Cover) by splitting existing classes into new classes that possess a better regional character by virtue of the climatic environment (latitude, proximity to the sea, topography). The leaf area index (LAI) from MODIS and normalized difference vegetation index (NDVI) from SPOT/Vegetation (a global monitoring system of vegetation) yield the two proxy variables that were considered here in order to perform a multi-year trimmed analysis between 1999 and 2005 using the K-means method. Further, meteorological applications require each land cover type to appear as a partition of fractions of 4 main surface types or tiles (nature, water bodies, sea, urban areas) and, inside the nature tile, fractions of 12 plant functional types (PFTs) representing generic vegetation types -principally broadleaf forest, needleleaf forest, C3 and C4 crops, grassland and bare land -as incorporated by the SVAT model ISBA (Interactions Surface Biosphere Atmosphere) developed at Météo France. This landscape division also forms the cornerstone of a validation exercise. The new ECOCLIMAP-II can be verified with auxiliary land cover products at very fine and coarse resolutions by means of versatile land occupation nomenclatures.

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Abstract. This work is part of the IDAF program (IGAC-DEBITS-AFRICA) and is based on the long-term monitoring of gas concentrations (1998)(1999)(2000)(2001)(2002)(2003)(2004)(2005)(2006)(2007) established at seven remote sites representative of major African ecosystems. Dry deposition fluxes were estimated by the inferential method using on the one hand surface measurements of gas concentrations (NO 2 , HNO 3 , NH 3 , SO 2 and O 3 ) and on the other hand modeled exchange rates. Dry deposition velocities (V d ) were calculated using the big-leaf model of Zhang et al. (2003b). The bidirectional approach is used for NH 3 surface-atmosphere exchange (Zhang et al., 2010). Surface and meteorological conditions specific to IDAF sites have been used in the models of deposition. The seasonal and annual mean variations of gaseous dry deposition fluxes (NO 2 , HNO 3 , NH 3 , O 3 and SO 2 ) are analyzed.Along the latitudinal transect of ecosystems, the annual mean dry deposition fluxes of nitrogen compounds range from −0.4 to −0.8 kg N ha −1 yr −1 for NO 2 , from −0.7 to −1.0 kg N ha −1 yr −1 for HNO 3 and from −0.7 to −8.3 kg N ha −1 yr −1 for NH 3 over the study period (1998-2007). The total nitrogen dry deposition flux (NO 2 +HNO 3 +NH 3 ) is more important in forests (−10 kg N ha −1 yr −1 ) than in wet and dry savannas (−1.6 to −3.9 kg N ha −1 yr −1 ). The annual mean dry deposition fluxes of ozone range between −11 and −19 kg ha −1 yr −1 in dry and wet savannas, and −11 and −13 kg ha −1 yr −1 in forests. Lowest O 3 dry deposition fluxes in forests are correlated to low measured O 3 concentrations, lower by a factor of 2-3, compared to other ecosystems. Along the ecosystem transect, the annual mean of SO 2 dry deposition fluxes presents low values and a small variability (−0.5 to −1 kg S ha −1 yr −1 ). No specific trend in the interannual variability of these gaseous dry deposition fluxes is observed over the study period.

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