13 kilometers
0.5m/km
Water erosion, mostly by streams and rivers that have a high gradient and discharge.
Because jet streams are above the friction layer, they have a negligible effect. The wind is balanced by the Coriolis effect and the pressure gradient so that the winds flow parallel to isobars.
Have to much water flow
All the time.
Species are modified to their specific environments, and that is why they are not identical all over the world.
Q-Tips
The steeper the gradient, the higher the velocity of flow.
In their headwaters, where the gradient is steep, most rivers cut into bedrock. These streams typically transport course particles that actively abrade the bedrock channel.
The discharge for a single stream should not change much from the headwater to the mouth. The exceptions to the mouth would be if another stream joined the main stream, which would increase the discharge or if you loose a significant amount of water to infilitration, which would decrease the discharge. The gradient should be high at the headwaters and gradually decrease downstream where it should be low at the mouth. Of course differences in lithologies or secondary streams can change the gradient for a short distance, thought the overall profile should fit the expected model.
the Mississippi headwaters is a kind of thing that is located in the Mississippi river. The Headwaters of a river are it's origins. The multiplicity of small streams that converge to form the main body of the river proper.
Temperature gradient seen nerby.
Polar jet streams
Polar jet streams
Polar jet streams
no there not
what are three factors that affect rate of stream erosion
Jet streams blow at speeds of 200 to 400 kilometers per hour.