start:hype_model_description:hype_land
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| Both sides previous revision Previous revision Next revision | Previous revision Next revision Both sides next revision | ||
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start:hype_model_description:hype_land [2020/04/29 10:24] cpers [Percolation] |
start:hype_model_description:hype_land [2020/04/29 10:31] cpers [Groundwater runoff] |
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| ({soillayerdepth(k)} - streamdepth) </m> | ({soillayerdepth(k)} - streamdepth) </m> | ||
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| + | 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. | ||
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| |{{: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.| | ||
| Line 292: | Line 294: | ||
| runoffd = trrcs * deltah / soillayerthick(k) * ep(k) | runoffd = trrcs * deltah / soillayerthick(k) * ep(k) | ||
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| + | 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:runoffthorughdrainagepipes.png?400|}}| | |{{:start:hype_model_description:runoffthorughdrainagepipes.png?400|}}| | ||
start/hype_model_description/hype_land.txt ยท Last modified: 2024/02/21 10:05 by cpers
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