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Polar low
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==History== Polar lows were first identified on the meteorological satellite imagery that became available in the 1960s, which revealed many small-scale cloud vortices at high latitudes. The most active polar lows are found over certain ice-free maritime areas in or near the [[Arctic]] during the winter, such as the [[Norwegian Sea]], [[Barents Sea]], [[Labrador Sea]] and [[Gulf of Alaska]]; however, polar lows also have been found in the [[Sea of Japan]] and the [[Sea of Okhotsk]]. Polar lows dissipate rapidly when they make landfall. [[Antarctic]] systems tend to be weaker than their northern counterparts since the air-sea temperature differences around the continent are generally smaller. Still, vigorous polar lows can be found over the [[Southern Ocean]].
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