WMS - Hazard information map Saxony (Atlas of...
Dataset description:
The hazard index map shows flood areas and intensities (water depth or specific discharge) during extreme floods for the Elbe river and waters of the 1st order in Saxony on an overview...
Source: Hazard information map of Saxony (Atlas of the flood hazard in Saxony)
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Additional Information
| Field | Value |
|---|---|
| Data last updated | unknown |
| Metadata last updated | June 17, 2023 |
| Created | unknown |
| Format | application/vnd.ogc.wms_xml |
| License | No License Provided |
| Conforms to | ["http://www.opengis.net/def/serviceType/ogc/wms"] |
| Created | 2 years ago |
| Download url | https://luis.sachsen.de/arcgis/services/wasser/gefahrenhinweiskarte/MapServer/WMSServer?request=GetCapabilities&service=WMS |
| Media type | application/vnd.ogc.wms_xml |
| Uri | urn:uuid:69a13a76-d2ef-cd4b-fd4f-cddfcee5afdc |
| Access services | [{"title": "WMS - Hazard map Saxony (Atlas of flood risk in Saxony)", "description": "The hazard map shows flood areas and intensities (water depth or specific discharge) in the event of extreme floods for the Elbe river and the waters of the 1st order in Saxony on an overview scale (1:100,000) with data from 2004. Extreme flooding (EHQ) is defined as an event that is significantly larger than HQ(100 ) is at least the highest observed event, but generally HQ(300). The flood areas were calculated without taking into account the effect of existing flood protection facilities, such as dams, dikes or polders. The intensity shown is \ Surfaces and extents represent an envelope of all possible flooding scenarios, i.e. not all represented areas are affected in a single event. This also applies if protective devices fail. In addition, the boundaries of the flooded areas at HQ(20) and HQ(100) are shown, also without taking into account the effect of flood protection facilities. Due to the various flooding and thus damage processes, a distinction was made between flat valley areas (free of bedload, mostly flooding that did not change the course) and steep areas (dynamic flooding with bedload transport, erosion and expected course change). Since the depth of flooding in the steep stretches of water can only indirectly provide information about the intensity and thus the hazard, the flow velocity on the forelands was also determined. The product of flood depth and flow velocity is shown as specific runoff (runoff per meter water width) for EHQ.", "endpoint_url": ["https://luis.sachsen.de/arcgis/services/wasser /hazard warning card/MapServer/WMSServer?request=GetCapabilities&service=WMS"], "serves_dataset": [], "uri": "https://geoportal.sachsen.de/md/4858d65f-0ed5-4bc8-ab8c-245313174db1"} ] |
| Access url | https://luis.sachsen.de/arcgis/services/wasser/gefahrenhinweiskarte/MapServer/WMSServer?request=GetCapabilities&service=WMS |
| Distribution ref | urn:uuid:69a13a76-d2ef-cd4b-fd4f-cddfcee5afdc |
| Id | a42101ed-6383-44f1-a542-912c7e1f91b3 |
| License | http://dcat-ap.de/def/licenses/dl-by-de/2.0 |
| Package id | d652a445-6d43-4b1f-91bc-bdbbf67b4769 |
| Position | 2 |
| State | active |