They occur at the boundaries between the first, second, and third wind systems
cool
thermal pollution
of course,evaporation can happen there
Unfiltered streams or lakes that may be contaminated by human or animal wastes are a common source of infection. Outbreaks can occur among campers and hikers who drink untreated water from mountain streams.
The two main types of jet streams are the polar jet streams and the subtropical jet streams. Polar jet streams are located at higher latitudes and are typically stronger, influencing weather patterns in mid-latitude regions. Subtropical jet streams, found at lower latitudes, occur at higher altitudes and generally have a more consistent flow. Both types play crucial roles in shaping weather systems and influencing climate.
Topsoil erosion is most likely to occur on the beds of lakes and streams. This is because the flow of water will pull the soil from the shore into the water.
Jet streams can occur at various altitudes, but the strongest and most well-known jet streams, like the polar jet stream and subtropical jet stream, typically occur at altitudes between 20,000 to 40,000 feet in the upper troposphere. These high-altitude, fast-flowing air currents play a significant role in influencing weather patterns.
Because the rivers and streams cannot handle the amount of rain that has fallen in a given period of time.
Jet streams are primarily categorized into two types: the polar jet streams and the subtropical jet streams. Polar jet streams occur at higher latitudes, typically between 30° to 60° latitude, and are associated with the boundary between cold polar air and warmer air from the south. Subtropical jet streams are found at lower latitudes, around 20° to 30° latitude, and are linked to the subtropical high-pressure systems. Additionally, there can be smaller-scale jet streams, such as the tropical jet stream, which can influence weather patterns in specific regions.
The average rainfall on rivers and streams can vary significantly depending on the location and climate of the region. Rainfall typically replenishes river and stream flow, providing a consistent source of water. Areas with higher average rainfall generally have more water flowing in rivers and streams compared to areas with lower average rainfall.
On the outer bank (at the tip of the meander)
Valleys occur between mountains and hills, typically formed by water erosion from rivers and streams over time. They are geographical low-lying areas that are usually longer than they are wide, with varying depths and widths.