Hello all,
I am trying to run a sub-daily streamflow routing.
Pcp data is hourly, the modelled streamflow is also expected to be hourly.
Used routing method: variable storage with green-ampt infiltration model.
my question is, i observe instability in the simulated streamflow.
Could it be due to a numerical instability in the hourly routing ? (CFL number overshooting?)
the precipitation data seem quite coherent so i ruled it out.
Herein attached a figure to display how the streamflow shoots after the year 2009.
this happens in almost every case (despite changing manning's, channel slope. etc).
Thanks
JJ