They're called jet-streams.
trade winds , prevailing westerlies, polar westerlies,doldrums
No, the strongest winds on earth occur inside very strong tornadoes. On rare occasion these winds can exceed 300 mph (480km/h).
by regions where the isobars are close together:D ...A+
Thunderstorms are dangerous storms that include lightning and can: Include powerful winds over 50 MPH; Create hail; and. Cause flash flooding and tornadoes
Polar Easterlies: From 60-90 degrees latitude.Prevailing Westerlies: From 30-60 degrees latitude (aka Westerlies).Tropical Easterlies: From 0-30 degrees latitude (aka Trade Winds).
jet streams
Jet Streams
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Jet Stream
Jet Stream
Jet Streams are narrow belts of high speed winds.
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.
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.
These narrow belts of strong winds, known as jet streams, are high-altitude air currents that flow in a concentrated path from west to east. They can impact weather patterns, air travel routes, and help transport heat and moisture around the globe. Jet streams play a key role in shaping the world's climate and weather systems.
The troposphere
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.
Narrow belts of high speed winds in the upper atmosphere are known as jet streams. These fast-flowing air currents can have significant influence on weather patterns and are commonly found near boundaries between warm and cold air masses. Jet streams are strongest in the wintertime when temperature contrasts are typically the greatest.