Stream discharge physically depends on two factors: stream cross-sectional area and velocity. Area is composed of width and depth. Q (flow) = vel x width x depth. Stream elevation change, or how steep a stream is, will affect the velocity. Higher sloping streams (like those with few meanders) will travel faster than sinuous, snaking streams that have a lower elevation drop per length of stream.
Stream discharge is a product of the velocity and the area of the stream (velocity x width x depth), and has units of volume per time (e.g. cubic feet per second, cubic meter per day, etc). Stream velocity is the vector describing the speed of the water and has units of length per time (feet per second, meter per second). Stream discharge is relatively constant as you move up and down a stream, while velocity will change predominately as you change depth. The velocity of water is lowest near the bed of the stream, and highest at the surface.
Stream erosion can be influenced by factors such as the volume and speed of water flow, gradient of the stream channel, presence of sediment or boulders, vegetation along the banks, and geology of the area. Human activities such as deforestation, urbanization, and construction of dams or levees can also significantly impact stream erosion.
A snake bite first affects the blood stream and the area immediately around the bite. If the snake is venomous, a raised infected area may raise up around the bite.
By deviding the multification of line pressure and screw dia with the crosssectional area of hydralic cylinder piston.
Stream deposition occurs when a flowing stream loses energy, causing it to slow down and deposit sediment that it was previously carrying. This commonly occurs when the stream enters a flatter area, like a floodplain or a lake. As the stream's velocity decreases, it can no longer transport sediment, leading to deposition.
By area do you mean cross sectional area of a stream tube? Bernoulli's principle only compares pressure and velocity and it covers all fluids. In the case of an ideal gas (constant density) decreasing the cross sectional area of a stream tube lets say; will not affect the pressure. But given any fluid volume..going from point a to point b if velocity decreases, particles in the fluid want to move outward. just remember any fluid must do two things move and apply pressure.
Q (Discharge in m3/s) = A (cross-sectional area in m2) x u (velocity - a corrected value in m/s)
The stream's catchment.
To determine velocity from an acceleration-time graph, you can find the area under the curve of the graph. This area represents the change in velocity over time. By calculating this area, you can determine the velocity at any given point on the graph.
It is because velocity is inversely proportional to the cross-sectional area. As the water runs down from the faucet it changes velocity because of the pull of gravity, hence the liquid will be narrower as it falls down the ground.
To find the position from a velocity-vs-time graph, you need to calculate the area under the velocity curve. If the velocity is constant, the position can be found by multiplying the velocity by the time. If the velocity is changing, you need to calculate the area under the curve using calculus to determine the position.