my mom said she dont know.
The carrying capacity of a stream is influenced by its discharge and velocity. A higher discharge and velocity typically allow a stream to transport larger sediments and materials downstream, increasing its carrying capacity. Conversely, lower discharge and velocity may limit the stream's ability to carry sediment and materials.
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.
Your question makes no sense, the center of mass of a storm is a spacial reference point and the peak discharge of a stream is a time. When rain falls on the ground, it takes time for the rain to accumulate and flow into a stream thus there is always a lage between the time of the rainfall and the build up of flow in the stream.
stream discharge is the amount of water flowing through a space OR increases between its source or mouth
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.
If in a given stream the velocity doubles, the discharge: Choose one answer
The lag time between peak rainfall and peak discharge on a hydrograph occurs because it takes time for water to travel through the watershed from where it falls as rain to the main channel of a river. Factors like soil type, topography, land use, and drainage patterns influence the flow pathways and the time it takes for water to reach the stream channel.
Q-Tips
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.