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Polar front jet stream, also called polar front jet or midlatitude jet stream, a belt of powerful upper-level winds that sits atop the polar front.
The polar front jet can be baroclinically unstable and break up into Rossby waves.
The polar front jet can be baroclinically unstable and break up into waves.
The polar front jet and the subtropical jet play a role in maintaining Earth's general circulation.
Unlike the polar front jet stream, it travels in lower latitudes and at slightly higher elevations, owing to the increase in height of the tropopause at lower latitudes.
The polar front jet moves in a generally westerly direction in midlatitudes, and its vertical wind shear which extends below its core is associated with horizontal temperature gradients that extend to the surface.
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It is best developed when the polar-front jet stream blows across the range.
Rossby wave, in meteorology, large horizontal atmospheric undulation that is associated with the polar-front jet stream and separates cold polar air from warm tropical air.
The air masses interact in the frontal systems commonly found embedded within the traveling cyclones that lie beneath the polar-front jet stream.
Over the Northern Hemisphere in the winter season, the polar-front jet stream is located above the midlatitudes (areas located between 30° and 60° N), with wind speeds varying between 193 and 402 km (120 and 250 miles) per hour.
The polar vortex over Antarctica and its adjacent seas is isolated from air outside the region by the polar-front jet stream in the Southern Hemisphere, which circulates between approximately 50° and 65° S over the Southern Ocean.
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