start:hype_model_description:hype_routing
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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_routing [2018/09/10 12:57] cpers [Common rivers processes] |
start:hype_model_description:hype_routing [2018/09/10 13:02] cpers [Common rivers processes] |
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| Line 72: | Line 72: | ||
| <m> ttpart = transtime - REAL(ttday) </m> | <m> ttpart = transtime - REAL(ttday) </m> | ||
| - | The inflow of the river is stored in two arrays (//riverq// and //riverc//) until it is time for it to drain out. The outflow is weighted by using the parts of the day that are during the time step. | + | The inflow of the river is stored in two arrays (//riverq// and //riverc//) until it is time for it to flow out of the river stretch. The outflow is weighted by using the parts of the time step (//ttpart//) that are to flow out during the time step. |
| transq = (1-ttpart)*riverq(ttday) + ttpart*riverq(ttday+1) | transq = (1-ttpart)*riverq(ttday) + ttpart*riverq(ttday+1) | ||
| Line 82: | Line 82: | ||
| ENDIF | ENDIF | ||
| - | After the calculation of outflow the values in the arrays are shifted forward one day. | + | After the calculation of outflow the values in the arrays are shifted forward one time step. |
| === Delay and attenuation === | === Delay and attenuation === | ||
start/hype_model_description/hype_routing.txt ยท Last modified: 2024/01/25 11:37 (external edit)
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