Hydrological attributes of terrains (Water Overlay): Difference between revisions
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|How fast this terrain can evaporate water from the underground. The {{inlink|weather}}'s evaporation speed is multiplied by this factor to determine the rate of evaporation. | |How fast this terrain can evaporate water from the underground. The {{inlink|weather}}'s evaporation speed is multiplied by this factor to determine the rate of evaporation. | ||
|- | |- | ||
|[[ | |[[Ground_infiltration_md_(Terrain)_(Water_Overlay)|GROUND_INFILTRATION_MD]] | ||
|m | |m/day | ||
| | |Surface | ||
|The | |The speed at which water can flow vertically from the surface to the underground unsaturated zone. | ||
|- | |- | ||
|[[ | |[[Ground_infiltration_md_(Terrain)_(Water_Overlay)|GROUND_INFILTRATION_MD]] | ||
| | |m/day | ||
|Underground | |Underground | ||
|The | |The speed at which water can flow vertically from the underground unsaturated zone to the underground saturated zone, and horizontally through across the saturated zone. | ||
|- | |- | ||
|[[Water_manning_(Water_Overlay)|WATER_MANNING]] | |[[Water_manning_(Terrain)_(Water_Overlay)|WATER_MANNING]] | ||
|s/(m<sup>1/3</sup>) | |s/(m<sup>1/3</sup>) | ||
|Surface | |Surface | ||
|The Gauckler–Manning coefficient of the | |The Gauckler–Manning coefficient of the terrain. | ||
|} | |} | ||
{{Template:WaterOverlay attribute nav}} | {{Template:WaterOverlay attribute nav}} |
Revision as of 13:19, 3 April 2019
Terrains in a project have a number of hydrological properties which can influence the flow of water in a project. Because there is always both surface and underground terrain defined for the entirety of the project area, all cells are affected by all properties of terrains, unless a construction is present with overwriting values.
Attribute | Unit | Terrain type | Description |
---|---|---|---|
WATER | boolean | Surface | Whether the specified terrain is a water terrain. |
ROOT_DEPTH_M | m | Surface | The depth of the roots of this surface terrain, relative to the surface. Water can be drawn from the underground and evaporated if the roots can reach it. |
WATER_EVAPORATION_FACTOR | factor | Surface | How fast this terrain can evaporate water from the underground. The weather's evaporation speed is multiplied by this factor to determine the rate of evaporation. |
GROUND_INFILTRATION_MD | m/day | Surface | The speed at which water can flow vertically from the surface to the underground unsaturated zone. |
GROUND_INFILTRATION_MD | m/day | Underground | The speed at which water can flow vertically from the underground unsaturated zone to the underground saturated zone, and horizontally through across the saturated zone. |
WATER_MANNING | s/(m1/3) | Surface | The Gauckler–Manning coefficient of the terrain. |