GitLab

The gathering of all outflow points from the atmopsheric grid and their catchments is now in a separate subrouting.

Improve the estimation of the distribution of the stream_topoindex by removing the HTUs which are at the source of the stream and thus no water in the stream.

Perform the triple HTU division over large confluence + rlen / rdz in the output are now the value for mainstream.

Test the dz limiter. It must now be between the minimum dz in the original data and the difference orogÃ_max and orog_min of the HTU.

Propose various metods to compute topoindex on the HTUs. The river length and elevation change within the HTU are not archived in the routing-graph file.

The river segment length and river segment elevation change per HTU is now carried until routing_reg_globalize. This allows to explore other methods of computing the topoindex.