BASEMENTBasic Simulation Environment for computation of environmental flow and natural hazard simulationLaboratory of Hydraulics, Hydrology and Glaciology (VAW)ETH Zurich |
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Hi,
I'm modeling a river arriving in a lake. When I have an inflow of 200m3/s I know that the outflow is at 430.5 msm. I have used a fixed water surface elevation with the intflow defined by a zhydrograph. I'm suprised because at the begining I have the following results:
TIME = 1.000003e+002 hyd. Time Step = 3.133820e-003
Qin[1] = 2.000000e+002 [m3/s] (Inflow)
Qout[2] = -1.100002e+003 [m3/s] (Outflow)
Is it because I have a dry initial condition? This means that there is water inflow from dowstream to upstream and after a certain time the water would go in the other direction?
Thank's for your help. Best regards
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Hi Quentin,
did I get you right: your INflow is a zhydrograph?
[...] with the intflow defined by a zhydrograph [...]
BASEd regards,
Daniel
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