Both tornadoes and the jet stream are weather patterns that involve strong winds, aside from that they are completely different.
The jet stream is located in the tropopause, which is the boundary between the troposphere and the stratosphere. It typically flows at high altitudes, around 10-15 kilometers above the Earth's surface.
a jet stream is important because of climate control
The curved shape of the jet stream is primarily influenced by the Earth's rotation and the temperature differences between air masses. The Coriolis effect, caused by the Earth's rotation, leads to the jet stream following a meandering path at high altitudes. Additionally, temperature contrasts between warm and cold air masses can create areas of low and high pressure, which further shapes the jet stream pattern.
Ferrel.
A jet stream of water shot out of the hose.
The jet stream travels between hot and cold air.
A continental jet-stream travels parallel to the equator - a polar jet-stream travels in a north/south direction.
A. The subtropical jet stream lies between the westerlies and polar easterlies; this statement is true. B. The polar jet stream typically flows to the east, while the subtropical jet stream flows towards the west.
The polar jet stream is generally stronger than the subtropical jet stream. The subtropical jet stream lies between the westerlies and trade winds.
The jet stream is located in the tropopause, which is the boundary between the troposphere and the stratosphere. It typically flows at high altitudes, around 10-15 kilometers above the Earth's surface.
The jet stream
The polar jet stream is generally stronger and faster-moving than the subtropical jet stream. The polar jet stream forms at higher latitudes and is located closer to the poles, while the subtropical jet stream is located at lower latitudes. The polar jet stream is associated with larger temperature contrasts and stronger pressure gradients, resulting in stronger winds compared to the subtropical jet stream.
mid latitude jet stream and jet stream
The jet stream is typically faster in the winter due to greater temperature contrasts between polar and tropical regions. This temperature difference creates stronger winds that drive the jet stream at higher speeds during the winter months.
jet stream
Wind doesn't control the jet stream; this is controlled by something much more complex. It has to do with the mass balance of the atmosphere, vertically propagating waves, and the earth's rotation.
The jet stream is strongest in the upper troposphere, which is the region of the atmosphere located between about 7 to 12 kilometers above the Earth's surface.