But the bigger the hole gets, the thinner the ozone layer will become over the rest of the earth. Then, there is the formation of Polar Stratospheric Clouds (PSCs). Below: Dangerous beauty. A polar winter vortex also forms in the Northern Hemisphere. During the continuously dark polar winter, the air inside the polar vortices becomes extremely cold, a necessary condition for polar stratospheric cloud formation. These are best observed during winters in more northerly latitudes. Meanwhile, chlorine concentrations build up during the polar winter, and consequent ozone destruction is greatest when the sunlight returns in polar winter . This means more dangerous UV radiation will reach the Earth's surface. Although polar stratospheric clouds can form in the Arctic, they rarely last long enough for extensive decreases in ozone. Polar stratospheric clouds (PSCs) are common in … "A 'warm' polar stratosphere is typically in the temperature range -73 o to -63 o C. Of course, as soon as the wave has dissipated, the polar region begins to cool down again." The polar vortex and polar stratospheric clouds exist only over Antarctica, which is why the ozone "hole" exists only there. Description. Polar stratospheric clouds (PSCs) are the exception. Polar stratospheric clouds (PSCs) are clouds in the winter polar stratosphere at altitudes of 15,000–25,000 m (49,000–82,000 ft). Though nacreous clouds are officially known as "polar stratospheric clouds", they are now common over Scotland, and have been observed as far south as the Midlands. Lower average winter temperatures in the upper atmosphere might explain why nacreous clouds seem to be appearing with increased frequency and distribution. Polar stratospheric clouds create the conditions for drastic ozone destruction, providing … Polar stratospheric clouds. However, in general, it is neither as strong nor as cold as the one that forms in the Antarctic. Figure Q10-2. They are best observed during civil twilight, when the Sun is between 1 and 6 degrees below the horizon, as well as in winter and in more northerly latitudes. While the clouds look amazing, they can be potentially quite dangerous to our planet. These beautiful images of polar stratospheric clouds were taken over Tromso City in Norway. Polar mesospheric clouds (PMCs) are a diffuse scattering layer of water ice crystals near the summer polar mesopause. The particles grow from the con-densation of water and nitric acid (HNO3). PSCs form during winters in the Arctic and Antarctic stratospheres. PSCs appear in the lower stratosphere near the poles in winter. This photo-graph of an Arctic polar stratospheric cloud (PSC) was taken from the ground at Kiruna, Sweden (67°N), on 27 January 2000. The nitric acid in polar stratospheric clouds reacts with chlorofluorocarbons to form chlorine, which catalyzes the photochemical destruction of ozone [3, 34]. 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