Ground bottom flow result type (Water Overlay): Difference between revisions
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|name=GROUND_LAST_SEEPAGE | |name=GROUND_LAST_SEEPAGE | ||
|icon=overlay_icon_water_ground_last_seepage.png | |icon=overlay_icon_water_ground_last_seepage.png | ||
|unit=m | |unit=m | ||
|mode=[[Result_type_(Water_Overlay)#Last_resulttype|Last]] | |mode=[[Result_type_(Water_Overlay)#Last_resulttype|Last]] | ||
|description=The amount of water that has seeped into the underground from a deeper layer below, raising the ground watertable. | |description=The amount of water that has seeped into the underground from a deeper layer below, raising the ground watertable. |
Revision as of 09:57, 15 January 2021
Icon | Result type | Unit | Mode | Description |
---|---|---|---|---|
File:Overlay icon water ground last seepage.png | GROUND_LAST_SEEPAGE | m | Last | The amount of water that has seeped into the underground from a deeper layer below, raising the ground watertable. |
¹ the units between () are as displayed in the 3D client. If exported to GeoTiff the SI-convention is used: meters (m) and seconds (s).
Any water on the surface is considered water stress. Open water is usually designed to function as a buffer for water, meaning an increase in the amount of water is not necessarily considered stress, unless the water level increases too much. "Too much" is defined by the ALLOWED_WATER_INCREASE_M attribute. As long as that amount of water is not exceeded, water stress in that location is considered 0.