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start:hype_model_description:hype_routing

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start:hype_model_description:hype_routing [2018/09/10 13:00]
cpers [Common rivers processes]
start:hype_model_description:hype_routing [2018/09/10 13:02] (current)
cpers [Common rivers processes]
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 <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 flow out of the river stretch. 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: 2018/09/10 13:02 by cpers