a streams discharge is the excess water from a storm or melted snow.
it is gradient, discharge and load.
Stream velocity is dependent of four things. They are, the flow type, the gradient, the channel shape, and the discharge of the stream. Streams will flow faster in narrow channels on steeper grades.
The slope or gradient of the stream is the most likely factor to affect the amount of erosion. Steeper slopes result in higher velocities, which in turn increase the erosive power of the stream. A steeper slope also allows the stream to carry larger sediment and potentially cause more erosion.
AnswerDischarge of material? Material discharged or eroded would increase with increasing slope due to the increased cutting action of the water.
A gulf stream is water ,and a jet stream is air.
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
Yea