Q (Discharge in m3/s) = A (cross-sectional area in m2) x u (velocity - a corrected value in m/s)
b the volume of water that flows over time
If in a given stream the velocity doubles, the discharge: Choose one answer
After a stream's discharge increases, it overflows its banks and a flood occurs.
In a typical stream where the gradient is steep the discharge is small.
In a typical stream where the gradient is steep the discharge is small.
The capacity of a stream is the maximum load it can carry. Capacity is directly related to a stream's discharge. The greater the volume of water in a stream is, the greater its capacity is for carrying sediment. So if a stream's discharge decreases, the stream's capacity also decreases.
After a stream's discharge increases, it overflows its banks and a flood occurs.
Water.
a discharge of a stream is the amount of water flowing past a certain point in a given unit of time.
In a typical stream where the gradient is steep the discharge is small.
Stream discharge would increase if additional water enters it, such as from a rain storm or from melting snow.
stream discharge is the amount of water flowing through a space OR increases between its source or mouth