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The polar vortex is a persistent, large-scale cyclone located near the Earth's poles, in the middle and upper troposphere and the stratosphere. It surrounds the polar highs and is part of the polar front. The vortex is most powerful in the hemisphere's winter, when the temperature gradient is steepest, and diminishes or can disappear in the summer. The Antarctic polar vortex is more pronounced and persistent than the Arctic one; this is because the distribution of land masses at high latitudes in the northern hemisphere gives rise to Rossby waves which contribute to the breakdown of the vortex, whereas in the southern hemisphere the vortex remains less disturbed. The Arctic vortex is elongated in shape, with two centres, one roughly over Baffin Island in Canada and the other over northeast Siberia.

The chemistry of the Antarctic polar vortex has created severe ozone depletion. The nitric acid in polar stratospheric clouds reacts with CFCs to form chlorine, which catalyzes the photochemical destruction of ozone. Chlorine concentrations build up during the winter polar night, and the consequent ozone destruction is greatest when the sunlight returns in spring (September/October). These clouds can only form at temperatures below about -80°C, so the warmer Arctic region does not have an ozone hole.

The Antarctic Polar Vortex typically lasts from August to November

Other astronomical bodies are also known to have polar vortices, including Venus, Mars, Jupiter, Saturn and Saturn's moon Titan.

Sources

"Polar vortex". European Environment Agency multilingual environmental glossary. Retrieved January 29. {{cite web}}: Check date values in: |accessdate= (help); Unknown parameter |accessyear= ignored (|access-date= suggested) (help)

"Polar vortex". Glossary of Meteorology. Retrieved January 29. {{cite web}}: Check date values in: |accessdate= (help); Unknown parameter |accessyear= ignored (|access-date= suggested) (help)

"World temperature gradient". Integrated Publishing: Aerographer/Meteorology. Retrieved January 29. {{cite web}}: Check date values in: |accessdate= (help); Unknown parameter |accessyear= ignored (|access-date= suggested) (help)

"What is the polar vortex?". The Weather Prediction.com. Retrieved January 29. {{cite web}}: Check date values in: |accessdate= (help); Unknown parameter |accessyear= ignored (|access-date= suggested) (help)

"The Antarctic Polar Vortex". Dynamics in the Ocean and Atmosphere. Retrieved January 29. {{cite web}}: Check date values in: |accessdate= (help); Unknown parameter |accessyear= ignored (|access-date= suggested) (help)

"The Polar Vortex and Arctic Weather Patterns". Arctic Climatology and Meteorology. Retrieved January 29. {{cite web}}: Check date values in: |accessdate= (help); Unknown parameter |accessyear= ignored (|access-date= suggested) (help)

"NASA Sees into the Eye of a Monster Storm on Saturn". Cassini-Huygens: News-Press Releases-2006. Retrieved November 12. {{cite web}}: Check date values in: |accessdate= (help); Unknown parameter |accessyear= ignored (|access-date= suggested) (help)

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	The '''polar vortex''' is a persistent, large-scale [[cyclone]] located near the Earth's [[poles]], in the middle and upper [[troposphere]] and the [[stratosphere]]. It surrounds the [[polar high]]s and is part of the [[polar front]]. The [[vortex]] is most powerful in the [[Sphere\|hemisphere]]'s winter, when the [[temperature gradient]] is steepest, and diminishes or can disappear in the summer. The [[Antarctic]] polar vortex is more pronounced and persistent than the [[Arctic]] one; this is because the distribution of land masses at high latitudes in the northern hemisphere gives rise to [[Rossby wave]]s which contribute to the breakdown of the vortex, whereas in the southern hemisphere the vortex remains less disturbed. The Arctic vortex is elongated in shape, with two centres, one roughly over [[Baffin Island]] in [[Canada]] and the other over northeast [[Siberia]].		The '''polar vortex''' is a persistent, large-scale [[cyclone]] located near the Earth's [[poles]], in the middle and upper [[troposphere]] and the [[stratosphere]]. It surrounds the [[polar high]]s and is part of the [[polar front]]. The [[vortex]] is most powerful in the [[Sphere\|hemisphere]]'s [[winter]], when the [[temperature gradient]] is steepest, and diminishes or can disappear in the [[summer]]. The [[Antarctic]] polar vortex is more pronounced and persistent than the [[Arctic]] one; this is because the distribution of land masses at high latitudes in the northern hemisphere gives rise to [[Rossby wave]]s which contribute to the breakdown of the vortex, whereas in the southern hemisphere the vortex remains less disturbed. The Arctic vortex is elongated in shape, with two centres, one roughly over [[Baffin Island]] in [[Canada]] and the other over northeast [[Siberia]].

	The chemistry of the Antarctic polar vortex has created severe [[ozone depletion]]. The nitric acid in [[polar stratospheric cloud]]s reacts with [[CFC]]s to form [[chlorine]], which [[catalysis\|catalyzes]] the photochemical destruction of [[ozone]]. Chlorine concentrations build up during the winter polar night, and the consequent ozone destruction is greatest when the sunlight returns in spring (September/October). These clouds can only form at temperatures below about -80[[Celsius\|°C]], so the warmer Arctic region does not have an ozone hole.		The chemistry of the Antarctic polar vortex has created severe [[ozone depletion]]. The nitric acid in [[polar stratospheric cloud]]s reacts with [[CFC]]s to form [[chlorine]], which [[catalysis\|catalyzes]] the photochemical destruction of [[ozone]]. Chlorine concentrations build up during the winter polar night, and the consequent ozone destruction is greatest when the sunlight returns in spring (September/October). These clouds can only form at temperatures below about -80[[Celsius\|°C]], so the warmer Arctic region does not have an ozone hole.