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The polar front jet stream

It is originated because of temperature difference.

It is associated with the polar front zone7 in each hemisphere (figure 23).

It runs at a more meandering path than the Sub Tropical Jet Stream

It extends between 40 and 60 latitudes in both Hemispheres.

It is found at a height between 6km and 9km in the atmosphere.

It swings towards poles in summers and towards equator in winter. When swinging to south it takes very cold air with it to subtropical region.