Polar cyclones are large-scale weather systems that form in the polar regions, characterized by low pressure and strong winds. These cyclones can occur in both the Arctic and Antarctic, typically during the winter months when temperatures are extremely low. They play a crucial role in the polar climate by redistributing heat and influencing sea ice dynamics. The structure of a polar cyclone includes a central eye, surrounded by a ring of clouds and precipitation. Unlike tropical cyclones, polar cyclones are less intense and do not have the same warm core. They can, however, lead to severe weather conditions, including blizzards and strong gusts, impacting local ecosystems and human activities.