Related Articles
Time-area method
This is a form of catchment routing model in which a hyetograph of rainfall is combined with a time-area diagram to produce a flow hydrograph. All of these must use the same time step, Dt. The procedure effectively divides a catchment into a number ...
Lag time (Lag factor)
In hydrology, catchment lag or delay has a general meaning, as the time taken for runoff in general to flow off a catchment to its outlet. It relates to the time difference between the centroids of the rainfall hyetograph and the runoff hydrograph. ...
Time of travel (time of entry, time of concentration)
Generally these names refer to the time required for water to flow from the farthest point on a catchment to its outlet during a storm, following flow paths dictated by natural topography and human changes. Times of flow are complex, since they ...
Storage routing calculations
These are carried out over a series of time steps, with the information obtained from solving equations at one time step being used as an input to the next step. In reservoirs, the information needed is: a relationship between storage and outflow, ...
Inflow Hydrograph (user-provided hydrograph) property sheet
This window enables you to enter a user-provided hydrograph at a pit. You have a choice of applying this above the inlet at the surface, or inside the pit. You need to specify the duration of this hydrograph and the time step between ordinates. This ...