The change in the Jet Stream is a warning signal of meteorological crises. What is the Jet Stream?
Jet streams are fast-flowing air currents in the atmosphere at altitudes of approximately 10,000 – 15,000 meters above the Earth's surface. Temperature differences between the polar regions and the equator cause them. Hot air from the equator rises and moves towards the poles, while cold air from the polar areas moves down to replace it. These hot and cold air masses swirl around each other in a large, tube-like, elliptical shape, blowing from west to east along the direction of the Earth's rotation. Jet streams move at high speeds, with velocities ranging from approximately 50 to 300 miles per hour. The central core of the jet stream has an average wind speed of 80 knots or 92 miles per hour. The average wind speed in winter can reach up to 300 miles per hour.
Jet streams are divided into two types:
The important roles of the jet stream
Reference: "Meteorological Department; The Meteorological Office; National Oceanic and Atmospheric Administration", Department of Climate Change and Environment.