Jet Streams
Jet Stream
The narrow belts of fast-moving air at higher levels of the atmosphere are called jet streams. These high-altitude, fast-flowing air currents typically occur at altitudes of about 10 kilometers (6 miles) and can significantly influence weather patterns and climate. Jet streams are primarily driven by the temperature differences between the equator and the poles.
The narrow belts of high-speed winds are called jet streams. These fast-flowing air currents are typically found in the upper levels of the atmosphere and play a significant role in influencing weather patterns and climate. Jet streams can vary in strength and position, often shifting with the seasons and affecting storm systems.
along colliding and subducting plate margins
Narrow belts of fast-moving air in the upper levels of the troposphere are known as jet streams. These currents typically flow from west to east and can significantly influence weather patterns by steering storms and affecting temperature distributions. Jet streams are typically found at altitudes of 6 to 12 kilometers (20,000 to 40,000 feet) and are strongest during winter months. Their position and intensity can vary, impacting global climate and localized weather events.
They're called jet-streams.
jet streams
Jet Stream
Jet Stream
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The narrow belts of winds that can reach 400 km are called jet streams. They are fast-flowing, narrow air currents found in the upper atmosphere, typically at altitudes of 7-16 km. Jet streams have a significant influence on weather patterns and can impact the movement of storms.
The two narrow belts of fast-moving winds are called the jet streams. They are located at high altitudes in the atmosphere, with the polar jet stream and the subtropical jet stream being the most prominent ones.
Jet Streams are narrow belts of high speed winds.
Jet streams are found in the upper troposphere - these are high velocity air flows that follow a curved path moving west-to-east around the globe.Narrow belts of strong winds are called jet streams. Jet streams blow near the top of the troposphere. The thin layer of air that surrounds the Earth is called the atmosphere.
Volcanoes occur in long, narrow belts because that's were the pate boundaries are.
The two narrow belts of fast-moving winds in each hemisphere are known as the Jet Streams. They flow high in the atmosphere at altitudes of around 10 kilometers and are influenced by temperature gradients between air masses. The Polar Jet Stream is found closer to the poles, while the Subtropical Jet Stream is located closer to the equator.
The Jet Stream