= GIS Structures = Three candidates are available for EDA When comparing surface layers for ECRINs and CCM for the bassin Loire-Bretagne : the CCM layer is more extended than the Ecrin Layer [[Image(source:EDA/data/Docs/trac/Loire Bretagne 1 - CCM Ecrins.jpg)]] == describing the CCM layers == gid:: id (corresponds to line number) wso1_id:: id of the primary catchment drained by the river segment. wso_id:: id of the Sea-outlet to which the river segment belongs. rvr_id:: reference of the name of the river to which the segment belongs (often 0) fromnode:: upstream node tonode:: downstream node strahler:: the stream order hierarchy, the sizes range from a first order stream to the largest a 11th order stream pfafstette:: Pfafstetter code (?) of the river segment and its primary catchment nextdownid:: next segment identifyer downstream points to wso_id longpath:: identifies wether the river segment is part of the longest flow path in the River Basin (sea-outlet), Y(es) or NULL maindrain_:: ? maindrain1:: ? length:: length of a river segment in meters cum_len:: cumulated length of the upstream flow network, including the river segment itself (longest route ?)-in meters pixels_100:: area directly drained by the river segment (area of the primary catchment), in 100m*100m grid-cells catchment_:: ? cont_pixel:: area upstream of the From Node drained by the river segment in 100m*100m grid-cells drain_km2:: full area drained by the river segment and upstream area - in square kilometres alt_gradie:: relief Energy of the river segment : ((Elevation at From Node-Elevation at ToNode)/Segment Length)*100 in per cent burned:: percentage grid-cells of the river segment having a high confidence level with respect to its geographical position confidence:: percentage of grid-cells of the river segment having a high confidence level with respect to its geographical position window:: here 2003 shape_leng:: ? the_geom:: the_geom [Image(source:"EDA/data/Docs/trac/Comparaison CCM-Ecrins-BDCarthage.jpg")]