Model attributes (Water Overlay)
The Water Overlay's model calculations depend on a number of calculation-wide parameters. These parameters are available as attributes of the water overlay and can be modified as such.
Extended reconstruction (Water Overlay)
Partial start sec (water Overlay) Partial end sec (water Overlay)
| Icon | Attribute | Unit | Range | Description | Default value |
|---|---|---|---|---|---|
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ALLOWED_WATER_INCREASE_M | m | The amount by which the water level on a water terrain must increase before it is considered stressed by water. This is used to compute the WATER_STRESS result type. | 0.4 | |
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AVG_SHORE_WIDTH_M | m | 0 to 10000 grid cells | With the surface water mode set to Grid Averaging, identified water average areas can be extended to include nearby shorelines within the configured distance. | 3 |
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AVG_TERRAIN_WIDTH_M | m | 0 to 10000 grid cells | With the surface water mode set to Avg Terrain, identified water average areas can be extended to include surrounding terrain within the configured distance. | 1000 |
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AVG_TERRAIN_STORAGE_M | m | 0 to 10000 | When determining the water level of a land cell that will be averaged, the level will ignore the part that is reserved for storage. | 0,05 |
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BREACH_MEASUREMENT_DISTANCE_M | m | Distance from the breach area to the automatically placed measurement point for the downstream water level of the breach, in the direction of the breach. | 100 | |
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BRIDGE_ELEVATION | nominal | 0 to 2 | Specifies the mode by which bridges are include in the elevation model, used for the water calculations. | Lowest |
| CULVERT_DEM_THRESHOLD_M | m | 0 to 10000 | The maximum distance a culvert's height can be below the terrain, for the terrain height to be adjusted to the threshold of the culvert. | 10 | |
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DESIGN_FLOOD_ELEVATION_M | m | Buildings in the model are assumed to have at most this height compared to the surface of the terrain. Greater values can create a more accurate model but will impact performance. | 1 | |
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GROUND_BOTTOM_DISTANCE_M | m | 0 to 10000 | Assumed distance under the surface terrain where the bottom boundary is situated. | 10 |
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GROUND_BOTTOM_PRESSURE_M | m | Optional: The additional head of higher areas outside the project causing water to flow in or out of the ground from deeper ground layers through the bottom boundary. | 0 | |
| GROUND_WATER | nominal value | Whether and how water in the ground is simulated during the calculation. | Infiltration Only | ||
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GROUND_WATER_DEPTH_M | m | -10000 to 10000 | The default depth of ground water in meters. | 1 |
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GROUND_WATERTABLE_WITH_SURFACE | boolean | Whether the ground watertable result type should also include the surface water level, when the groundwater levels are close to the surface. | True | |
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HYDRAULIC_CONDUCTIVITY_WITH_THICKNESS | boolean | When selected, the Terrain value HYDRAULIC_CONDUCTIVITY_WITH_THICKNESS_MD is used for horizontal groundwater flow calculations, otherwise HYDRAULIC_CONDUCTIVITY_MD is used. | 0 | |
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IMPACT_FLOOD_THRESHOLD_M | m | The amount of water a Building must experience before it is considered impacted by water. | 0,1 | |
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IMPACT_RANGE_M | m | the width in meters of the water next to or against the building that have to be flooded before the building is considered impacted by water. | 3 | |
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INCREASED_RESOLUTION | boolean | Load the DEM at twice the resolution. | False | |
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INFILTRATION_FACTOR_S | factor | -10 to 10 | This value is multiplied with the surface infiltration speed and can be used to adjust the infiltration over time. Default is 1 (no adjustment). | 1 |
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LIMIT_AREA | nominal value | Whether and how calculations in the simulation should be limited to specific locations of the project area. | 0 (Entire map) | |
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LIMIT_RAIN | nominal value | Whether rainfall can be overridden by rainfall defined in rain areas across the project area. | 0 (Entire map) | |
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MAX_INFILTRATION_M | m | Assumed maximum amount of infiltrated water that can be stored in the ground layer below non-water cells. | 1 | |
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MAX_WATER_BOTTOM_M | m + datum | The maximum height for the bottoms of water terrains. Any water terrain with a bottom at a higher datum height has its bottom lowered to this value. | 10000 | |
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MICRORELIEF_STORAGE_FRACTION | fraction (m/m) | 0.0 to 1.0 | Storage Fraction defines how much space is between Microrelief hills that can be used to store water. Setting this value to zero disables the Microrelief functionality all together. | 1.0 |
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MIN_MAX_ELEVATION | Nominal value | 0 to 2 | Whether to use highest and lowest elevations found for a grid cell for land and water respectively when interpreting the elevation model. | 1 |
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OBJECT_ENTRY_CORRECTION | cells | 0 to 3 cells | How many cells allowed to move a hydraulic structure's entry point when it overlaps with another hydraulic building. | 2 |
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PREQUEL_SURFACE_LEVEL_RELATIVE | boolean | Whether the SURFACE_LEVEL prequel is considered relative instead of a datum height. | 0 | |
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RISE_RATE_DISTANCE_M | m | 0 to 10000 | The water height threshold for computing the Flood rise rate result type. | 1.5 |
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SEWER_OVERFLOW_THRESHOLD | fraction (m/m) | 0 to 1 | How much of a sewer's storage must be filled with water before the sewer overflows are allowed to overflow water. | 0.9 |
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SHORELINE | Nominal value | 0 to 2 | Whether to automatically fill cells near a water terrain when there is a mismatch between the extend of the water terrain and the DEM. | 1 |
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DURATION_MIN_LEVEL_M | m | -10000 to 10000 | The amount of water which must be exceeded in a specific location before the duration of surface water can be recorded. This is used to compute the SURFACE_DURATION result type. | 0 |
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STABILIZER_ANGLE | angle (0-90°) | 0 to 90 | A partly flooded cell (especially at the edges of waterways) can become unstable when the angles in X and Y direction are too far apart. In this case the fluxes in U and V cannot easily be resolved mathematically while preserving balance. To prevent unrealistic fluxes from appearing, only the flux in the primary direction will be preserved. A stabilizer angle of zero means that all cells can be considered partly flooded cells, while an angle of 90 degrees will disable the stabilizer. | 10 |
| START_DATE_MS | long | The date and time which is considered the starting moment of the simulation. | 0 | ||
| SURFACE_WATER | Nominal value | Whether and how water on the surface is simulated during the calculation. | Shallow | ||
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SURFACE_WATER_EVAPORATION_FACTOR | factor | 0 to 10 | The factor by which the weather evaporation factor is multiplied to compute the amount of evaporation which takes place on the surface. | 1.3 |
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TIMEFRAME_TIMES | integer | 0 to | The time of individual timeframes in seconds relative to the start date of the simulation. | 0 |
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TIMEFRAMES | integer | 1 to 1000 | The number of intermediate results recorded during the calculation. Each timeframe becomes a snapshot of data which can be viewed and analysed. | 10 |
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UNSATURATED_FRACTION | fraction | The initial fraction of the maximum storage capacity of the unsaturated zone which is filled with water. | 0.0 | |
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WEIR_DAM_MULTIPLIER | factor | The width with which the weir's dam should be generated perpendicular to it's direction, relative to its flow width. | 4 | |
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WEIR_MOVE_INTERVAL_S | seconds | 0 to 3.4028235E38 | Interval between Weir height adjustments in seconds. The Weir moves up/down to reach the target upstream water level. | 10 |
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WEIR_MOVE_STEP_M | m | When the move interval has passed the Weir height is adjusted up/down by this step distance in meters. | 0.01 | |
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WEIR_MOVE_RANGE_M | seconds | 0 to 3.4028235E38 | When the Weir height is adjusted up/down it is clamped by this value in meters. | 0.5 |











