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Documentation
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About
- Getting Started & Use Cases
- Support
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What's New
- DynamicFlood now available in Great Britain
- Global contour maps now available
- Updated Swedish topsoil map
- Scalgo Live Global theme is updated with new elevation and land cover data
- Detailed culvert information in DynamicFlood
- No more Lantmäteriet fees for Swedish data
- Depth-dependent surface roughness (Manning) in DynamicFlood
- Detailed land cover map for all of Great Britain
- National French high-resolution land cover map
- Work with multiple features simultaneously in the canvas
- Spill points on flash flood map and depression map
- New surface roughness (Manning) parameters for DynamicFlood
- Workspace and Modelspace sharing updates
- Regionally varying rain in DynamicFlood Sweden
- Veden imeytyminen nyt osana rankkasadeanalyysejä
- Use Scalgo Live anywhere in the world
- DynamicFlood: Live model speed info and regionally-varying rain events
- Sea-level rise: Download building flooding information
- Detailed contour maps and editable buildings in Workspaces
- New in Modelspaces: Explore hydrodynamic simulations and visualise the dynamics of flow velocity
- National German high-resolution land cover map
- Specify basins and protrusions by drawing their outer boundary
- Simplified path features
- National Norwegian high-resolution land cover map
- Organise and communicate on a digital canvas
- New sidebar to help organize your analyses and queries
- Sliding contours
- Ny skyfallsanalys och en ännu bättre marktäckekarta
- New land cover map for Finland
- Depths in the depression map
- New Danish land cover map with more classes
- National Swedish High-Resolution Impervious Surface Mapping
- Watershed tool updated with even better descriptions of catchment characteristics
- National Flash Flood Map with Infiltration and Drainage for Denmark
- Add your own WMS layers to SCALGO Live
- Enriched building data in Denmark
- National hydrological corrections and Land Cover for Poland
- National hydrological corrections for Norway
- Updated Impervious Surface Mapping for Denmark
- National hydrological corrections and updated local data for Finland
- Fast and intuitive tools to work with infiltration and land use
- Improvements to vector imports and exports
- National Danish groundwater model
- New Sweden high-resolution model
- New powerful depression map and more analyses visualization options
- Introducing Modelspaces: Get your hydrodynamic models into SCALGO Live
- Use case videos
- Access a EA flood maps inside SCALGO Live
- Improved map export
- New powerful ways to edit the elevation model
- Better coloring of flooding layers and sea-level depth filtering
- National Danish High-Resolution Impervious Surface Mapping
- National access for local and regional organizations
- Simpler, more powerful downloads
- Customize Layer Transparency
- Hydrological corrections and new data in Sweden
- Improved export functionality
- Access a wide range of authorative data inside SCALGO Live
- Importing VASP data
- Measure gradients, undo edits, and Norway updates
- New terrain edit features, soil balance information and much more...
- Browse historical orthophotos in SCALGO Live
- Emergency planning with sea-level rise from national forecast data
- Detailed information about watershed composition
- Better styling of imported vector layers
- New Danish Elevation Model
- Work with gradients in the profile widget
- Flood risk screening from rivers and flow paths
- New workspace tool: Raise and lower terrain uniformly
- Importing LandXML TINs, LAS point clouds
- New model in Sweden
- Side slopes on workspace features
- Drag and drop enhancements
- Swedish contour maps
- Subsurface basins and sewage drains in workspaces
- New Interface
- Volume information for watersheds and flow paths
- New powerful tool for emergency response and coastal flood prevention
- Denmark: New flash flood map
- Sweden: Geodatasamverkan setting for Swedish users
- Import custom terrain models
- New Hydrological Corrections
- Elevation contours now available
- Download orthophotos as JPEG and PNG
- Subsurface structures in workspace
- Sea-levels in terrain profiles
- Updated orthophotos
- Models and analysis update
- User interface updates
- User interface updates
- GeoDanmark/FOT data, Matrikelkortet now available
- New flash flood map
- Download of risk polygons
- Updated orthophotos
- Nationwide hydrology on the new DHM/2015 model now available
- New flash flood map computation available with watershed download
- DHM/2015 variants and sea-levels now available nationwide
- DHM/2015 now available nationwide
- Hydrology on the new DHM/2015 model now available
- New DHM/2015 Model - now with buildings
- New DHM Model
- Watershed Tool
- Ad hoc layers
- Nationwide contour maps for all countries
- Single Sign-On
- Data Fees
- User Interface
- Canvas
- Analysis
- Workspaces
- Core+ DynamicFlood
- Core+ NatureInsight
- Streams and Flow
- Modelspaces
- Physical Properties
- Country Specific
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About
Country Specific – Great Britain
National LIDAR Programme
Cell Size | 1x1 m |
Coordinate System | BNG |
Vertical Reference | OS Newlyn Datum |
Flight Years | 2016–2021 |
Our elevation model of Great Britain is based primarily on open LIDAR composite DTM models made available by the Environment Agency, Natural Resources Wales, and the Scottish Environment Protection Agency. The Environment Agency National LIDAR Programme started in November 2016 and aims to have coverage of all of England by 2021. We strive to keep our model up to date with the latest sources.
In order to use an elevation model for hydrological analysis such as watershed and flow accumulation computations, two primary conditions need to be met:
- The upstream area of any river should be covered by the elevation model.
- Structures on top of the terrain should only be present in case they actually block water from flowing under or through them.
Below, we discuss how we process the model to fulfill these conditions as well as possible.
Extensions
In order to cover all of England, Wales and Scotland, we have extended the open LIDAR data from the UK government in the following areas:
- For the parts of England not yet covered by the National LIDAR Programme, we have used the older Environment Agency 1m DTM, and for parts not covered by the 1m DTM we have used the 2m DTM.
- For the parts of Wales not covered by the Wales 1m DTM, we have used the Wales 2m DTM.
- For the parts of Scotland not covered by the LiDAR for Scotland Phase 4 DTM, we have used the Phase 3, Phase 2 or Phase 1 DTM, as well as Environment Agency's "LIDAR Composite DTM for Scotland".
- For the parts not covered by open LIDAR datasets mentioned above, we use the 30-meter EU-DEM dataset, which in turn is based on SRTM and ASTER GDEM data.
A full overview of which data source is used for which part of the model is available clicking the gear icon next to an elevation layer, selecting the "Source" tab, and "Show source information". Use the point query tool to highlight a coverage area and see the name of the source.
Bridges and underpasses
Major bridges have generally been removed from the models delivered by the Environment Agency, making most bigger rivers able to flow freely to the sea. However, for many smaller bridges and underpasses, additional "hydrological corrections" may be necessary. These can e.g. be made through workspaces in SCALGO Live.

Apart from vegetation and major bridges, also buildings have been removed from the terrain model during construction. When computing water flow paths, more realistic results are generally obtained when the elevation model does include buildings so water can be simulated to flow around them. In SCALGO Live, we accomplish this by adding buildings back into the model using a dataset of building footprints, where we raise all grid cells covered by a building to a height 10 meters above the highest terrain point within the building footprint. This model is called "Terrain/Buildings" and is the basis for all nationwide hydrological computations.
The building footprints are taken from the Ordnance Survey OpenMapLocal Building dataset.

Rivers
Major rivers have been lowered in the elevation model to ensure that water can flow freely to the coast. The river lines are taken from the Ordnance Survey Open Rivers dataset.

Coastline
We have removed parts of the LIDAR models that are off the coast, as the data is generally unreliable. The coastline is taken from the Ordnance Survey Open ZoomStack vector dataset, layer named "Land".
Land Cover
The SCALGO land cover map is available in the UK. For more information, please consult the land cover section of this documentation.
Base map and aerial photography
The default map view when you go to SCALGO Live shows the Ordnance Survey Open ZoomStack map, rendered in the "Outdoor" style. Other map styles are available through the gear menu on the "Base Map" layer. The street names and place labels are sourced from OpenStreetMap. You also have the option of viewing Aerial photography provided by Mapbox.
Rain events
Design rain events in the United Kingdom are based on the PXR-2 dataset (Parametrized eXtreme Rain), a global gridded product developed by Courty et al. (2019). PXR-2 provides Generalized Extreme Value distribution parameters for deriving intensity–duration–frequency (IDF) curves at a spatial resolution of approximately 31 km. For design rainfall estimation in the UK, we extract rainfall depths for a 4-hour event duration and return periods from 2 to 500 years.
We generate design hyetographs using a storm profile developed specifically for the UK by CEH (Center for Ecology and Hydrology) as part of the ReFH2 (Revitalised Flood Hydrograph) model framework. We use the summer storm profile, which represents convective rainfall patterns observed in the UK during summer months. The profile defines how the total rainfall depth is distributed over the event, with the peak intensity occurring at the midpoint.
Please note that the PXR dataset generally underestimates rainfall intensities compared with the intensities prescribed by ReFH2, especially for shorter durations (<24 hr).
Soil type
The soil type map used in Scalgo Live UK is based on the Soil Parent Material Model from BGS. Specifically, we use the soil texture layer, and map the classes found in that layer to our USDA-based topsoil typology according to the table below. For more information about the Scalgo soil type classes and how we enhance the topsoil map, see the soil type documentation.
BGS SOIL_TEX | Topsoil type |
CLAYEY LOAM TO SANDY LOAM | Clay loam |
CLAYEY LOAM TO SILTY LOAM | Clay loam |
LOAM TO SANDY LOAM | Loam |
SAND TO SANDY LOAM | Sandy loam |
LOAM TO CLAYEY LOAM | Clay loam |
PEAT | Gyttja/peat |
SAND TO LOAM | Loam |
LOAM TO CLAY | Clay |
CLAY TO SANDY LOAM | Clay |
CLAY TO CLAYEY LOAM | Clay |
LOAM TO SILTY LOAM | Silt loam |
CHALKY, SILTY LOAM | Silt loam |
LOAM TO CLAYEY LOAM, LOCALLY CHALKY | Clay loam |
CLAY TO LOAM | Clay |
LOAM | Loam |
CLAYEY LOAM | Clay loam |
CLAY TO SILT | Clay |
SANDY LOAM TO SAND | Sandy loam |
SILTY LOAM | Silt loam |
SILTY LOAM TO SANDY LOAM | Silt loam |
SILTY LOAM TO SILT | Silt |
SANDY LOAM | Sandy loam |
CHALKY CLAY TO CHALKY LOAM | Clay |
SAND | Sand |
SANDY LOAM TO CLAYEY LOAM | Clay loam |
SILT TO SAND | Silt |
CLAYEY LOAM, LOCALLY CHALKY | Clay loam |
LOAM TO SILTY | Silt |
NA | Clay |
SILT TO SILTY LOAM | Silt |
PEATY CLAY | Gyttja/peat |
CHALKY, SANDY LOAM | Sandy loam |
SANDY LOAM TO LOAM | Loam |
LOAM TO SANDY | Loam |
VARIED, LOCALLY PEATY | Gyttja/peat |
SANDY LOAM TO SILTY LOAM | Silt loam |
CLAYEY | Clay |
SAND TO SILT | Silt |
PEATY CLAY OR SILT | Gyttja/peat |
PEAT AND PEATY CLAY OR SILT | Gyttja/peat |
PEATY SILT | Gyttja/peat |
Urban and sewered areas
To determine whether an area is to be considered sewered (affecting the fate of all water on artificial surfaces in DynamicFlood) we use the map Built Up Areas from Ordnanace Survey (can be found in the Library). We assume that all areas that fall within a polygon in this map have a sewer system, and that all areas that fall outside these polygons do not have any sewer system.
We set the maximum capacity of the sewer system in DynamicFlood in Great Britain to 20 mm/hr. This value was chosen to reflect common historical dimensioning practice in Great Britain.
To determine whether an area is to be considered urban (affecting some soil types in the Topsoil map), we use the same map as for sewered areas.