Surface water - salinisation lines
Description
At low discharge of the Rhine or due to a high water level at sea (by storm), salt water from the Nieuwe Waterweg can enter the main water system. As a result, inlet points can become salinised. These lines are an indication of where salinisation may occur
Resources
| Name |
Format |
Description |
Link |
|
0 |
|
https://geodata.zuid-holland.nl/geoserver/water/wms?service=WMS&version=1.3.0&request=GetCapabilities |
|
0 |
|
https://geodata.zuid-holland.nl/geoserver/water/wfs?service=WFS&version=2.0.0&request=GetCapabilities |