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.
The jet stream is located in the tropopause, which is the boundary between the troposphere and the stratosphere. It typically flows at high altitudes, around 10-15 kilometers above the Earth's surface.
The jet stream is located in the tropopause, which is the boundary between the troposphere and the stratosphere. It is a fast-flowing, narrow air current that moves from west to east at high altitudes.
The curved shape of the jet stream is primarily influenced by the Earth's rotation and the temperature differences between air masses. The Coriolis effect, caused by the Earth's rotation, leads to the jet stream following a meandering path at high altitudes. Additionally, temperature contrasts between warm and cold air masses can create areas of low and high pressure, which further shapes the jet stream pattern.
The convection cell that connects the polar jet stream and the subtropical jet stream is known as the Ferrel Cell. This cell operates between the polar cell and the Hadley cell, facilitating the movement of air and influencing weather patterns. The Ferrel Cell plays a crucial role in the dynamics of the mid-latitude atmosphere, where it helps to transfer energy and moisture between these two jet streams.
Woah, that's a good question. Maybe the air stream? Or the plane 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 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.
my mom said she dont know.
If in a given stream the velocity doubles, the discharge: Choose one answer
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.
The carrying capacity of a stream refers to the maximum amount of sediment and material it can transport, which is influenced by its discharge and velocity. Higher discharge increases the volume of water flow, allowing the stream to carry more sediment. Similarly, greater velocity enhances the stream's ability to lift and carry particles, increasing its overall carrying capacity. Therefore, both discharge and velocity are critical factors that determine how much material a stream can transport.
Q-Tips
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.
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.
After a stream's discharge increases, it overflows its banks and a flood occurs.