AbstractBroadCrestedCWeir_delhs Field

Linear flow variation. For water level differences less than delhs use a linear Q variation between h1-h2=delhs and h1-h2=0. This is to avoid stability problems for small water level differences where dQdh goes to infinity. Unit: [m] Default: 0.01

protected double _delhs

Protected _delhs As Double

protected:
double _delhs