Velocity refers to the speed of water flow in a river, typically measured in meters per second. Volume, on the other hand, refers to the amount of water passing through a given point in the river over a period of time, usually measured in cubic meters per second. In essence, velocity is the speed of the water flow, while volume is the quantity of water flowing through a specific section of the river.
The velocity of a river is the speed at which the water in the river is flowing in a particular direction. It is typically measured in meters per second or feet per second. Velocity can vary at different points along a river depending on factors such as stream gradient, channel width, and flow volume.
Average velocity increases downstream because of the overall flow of the river. As the river moves in the downstream direction, the volume of water increases due to tributaries adding water along the way. This increase in water volume results in a higher average velocity as the same amount of water needs to flow through a larger channel.
Discharge is the volume of water flowing in a river at a certain point over a specific period of time, usually measured in cubic meters per second. It directly affects velocity in rivers because as discharge increases, the amount of water flowing through the river also increases, leading to higher velocity. Conversely, lower discharge results in slower velocities.
Increasing the gradient or slope of the river bed is most likely to increase the velocity of a river. This change allows water to flow more rapidly downhill, resulting in higher velocity.
To find the magnitude of the velocity vcr of the canoe relative to the river, you can use vector addition. Add the velocity of the canoe with respect to the water (vcw) to the velocity of the water with respect to the river (vwr). The formula is vcr vcw vwr.
The velocity and discharge volume of the stream or river.
The velocity of a river is the speed at which the water in the river is flowing in a particular direction. It is typically measured in meters per second or feet per second. Velocity can vary at different points along a river depending on factors such as stream gradient, channel width, and flow volume.
These obstacles causes friction between water and rocks.This ultimately reduces the velocity of river water.The more roughness of the channel, the less the river`s velocity.
The difference is width
The velocity of the river increases downstream due to the cumulative effect of gravity pulling the water downhill. As the river flows downstream, it collects water from tributaries and gains more volume, leading to an increase in velocity to accommodate the larger volume of water. Additionally, friction between the water and riverbed is reduced downstream, allowing the water to flow more freely and pick up speed.
Take the elevation from an upstream point on the river and the elevation from a point downstream on the river. Calculate the difference in the two elevations. Measure the distance between the two points by tracing the path of the river. Divide the difference in the two elevations by the distance between the two points in order to get the slope of the river, or the river gradient.
A river's power to erode depends on its flow velocity, the volume of water it carries, the type and size of sediment it transports, and the slope of the river channel. These factors influence the force and effectiveness of erosion by the river.
A river's power to erode depends on the gradient, the volume and velocity, and the quantity of erosive burden. A river will normally move outwards on bends, deepening the farthest channel, and thus increasing the erosion on that bank.
The difference between a river and a stream is the name applied to it by local residents, and relative size. In the same region, something called a river is usually larger than something called a stream. However, something that is called a river in one place could be the same size as something called a stream in another place.
we don
Average velocity increases downstream because of the overall flow of the river. As the river moves in the downstream direction, the volume of water increases due to tributaries adding water along the way. This increase in water volume results in a higher average velocity as the same amount of water needs to flow through a larger channel.
Manning equation if the hydraulic radius decreases then the velocity decreases