start:hype_model_description:hype_land
Differences
This shows you the differences between two versions of the page.
| Both sides previous revision Previous revision | Next revision Both sides next revision | ||
|
start:hype_model_description:hype_land [2020/04/29 10:30] cpers [Runoff through drainage pipes] |
start:hype_model_description:hype_land [2020/04/29 10:31] cpers [Groundwater runoff] |
||
|---|---|---|---|
| Line 237: | Line 237: | ||
| ({soillayerdepth(k)} - streamdepth) </m> | ({soillayerdepth(k)} - streamdepth) </m> | ||
| | | ||
| + | If the frozen soil model is used, it influences in two ways; one, the water available for runoff is reduced to the liquid fraction, and two, the frozen water is assumed to expand possibly increasing the water level in the soil. | ||
| + | |||
| |{{:start:hype_model_description:runofffromthird_layer.png?400|}}| | |{{:start:hype_model_description:runofffromthird_layer.png?400|}}| | ||
| |Figure 6: Runoff from the third soil layer with a stream.| | |Figure 6: Runoff from the third soil layer with a stream.| | ||
start/hype_model_description/hype_land.txt ยท Last modified: 2024/02/21 10:05 by cpers
Except where otherwise noted, content on this wiki is licensed under the following license: CC Attribution-Share Alike 4.0 International
