Stream discharge would increase if additional water enters it, such as from a rain storm or from melting snow.
An increase in precipitation, snowmelt, or glacial melt can cause a stream's discharge to increase. Additionally, if there is a sudden influx of water from a tributary or a dam release upstream, it can also lead to an increase in stream discharge.
After a stream's discharge increases, it overflows its banks and a flood occurs.
increase
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When the discharge of a stream increases, so does it's velocity. When it decreases, so does the velocity.
The carrying capacity of a stream is influenced by its discharge and velocity. Higher discharge and faster velocity can increase the stream's ability to transport sediment and debris, thus raising its carrying capacity. Conversely, lower discharge and slower velocity may result in a reduced carrying capacity as the stream has less energy to move material.
rate of stream discharge is directly proportional to the erosion i.e the higher the velocity of the stream then it will erode the rock rapidly while the deposition process will be slow when the velocity will be high.
If in a given stream the velocity doubles, the discharge: Choose one answer
The carrying capacity of a stream refers to its ability to transport sediment. Higher discharge and velocity typically increase a stream's carrying capacity as they provide more energy to move sediment. However, if the stream's carrying capacity surpasses its available sediment, deposition can occur.
The discharge of a stream is directly affected by the slope of the stream channel. A steeper slope will generally result in a higher discharge due to increased velocity and energy to transport water. Conversely, a gentler slope will result in lower discharge.
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.