a streams discharge is the excess water from a storm or melted snow.
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.
A stream's ability to erode mainly depends on its discharge (volume of water flow), velocity (speed of flow), and the amount of sediment carried in the water. Higher discharge and velocity typically result in increased erosion potential.
The ability of a stream to erode and transport material largely depends on its discharge, velocity, gradient, and the size and shape of the sediments. These factors influence how much sediment a stream can carry and how effectively it can erode material from its surroundings.
The land area that contributes water to a stream is known as its watershed or catchment area. This area collects rainfall and other sources of water, which then flow into the stream through surface runoff or groundwater discharge. The health and size of the watershed can significantly impact the quantity and quality of water in the stream.
Stream velocity refers to the speed at which water flows in a stream or river. It is typically measured in meters per second or feet per second and can vary depending on factors such as channel geometry, slope, and discharge. Stream velocity is an important parameter in hydrology and river engineering for understanding water movement and erosion processes.
If in a given stream the velocity doubles, the discharge: Choose one answer
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.
After a stream's discharge increases, it overflows its banks and a flood occurs.
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 is the amount of water flowing through a space OR increases between its source or mouth
Stream discharge would increase if additional water enters it, such as from a rain storm or from melting snow.
Yea