In the upper course of a river, there is a V-shaped valley with a steep gradient as the water is constantly using up the majority of its energy to overcome friction. As a river flows downstream, the valley becomes a U-shape and the gradient decreases. This is because there is less gravitational pull towards the sea/lake level. Also towards the middle and lower courses, there are more tributaries and confluences which will add more discharge to the river basin. This is constantly happening and thus, as it flows downstream it increases. The velocity also increases as there is more discharge.
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.
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.
Discharge refers to the volume of water flowing in a river or stream. When discharge increases, the speed and force of the water also increase, leading to greater erosion of the earth's surface. The increased volume of water can carry more sediment and particles, allowing it to erode and transport more material, shaping the landscape over time.
a streams discharge is the excess water from a storm or melted snow.
Stream temperature can increase due to various factors such as reduced shade from vegetation, urbanization leading to heat absorption from impervious surfaces, discharge of warm water from industrial processes or power plants, and climate change impacting overall temperature patterns. Additionally, changes in water flow and depth can also influence stream temperature.
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.
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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.