Precipitation cloud? no Classification Other Minimum altitude (feet) 49,000 | Indicates precipitation No Abbreviation PSC Maximum altitude (feet) 82,000 | |
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Appearance Glowing brightly with vivid iridescent colors | ||
C22 polar vortex ozone hole ozone depletion polar stratospheric clouds geography environment
Polar stratospheric clouds or PSCs, also known as nacreous clouds (/ˈneɪkriː.əs/, from nacre, or mother of pearl, due to its iridescence), are clouds in the winter polar stratosphere at altitudes of 15,000–25,000 meters (49,000–82,000 ft). 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. They are implicated in the formation of ozone holes. The effects on ozone depletion arise because they support chemical reactions that produce active chlorine which catalyzes ozone destruction, and also because they remove gaseous nitric acid, perturbing nitrogen and chlorine cycles in a way which increases ozone destruction.
Contents
- C22 polar vortex ozone hole ozone depletion polar stratospheric clouds geography environment
- Polar stratospheric clouds
- Formation
- Types
- References
Polar stratospheric clouds
Formation
The stratosphere is very dry; unlike the troposphere, it rarely allows clouds to form. In the extreme cold of the polar winter, however, stratospheric clouds of different types may form, which are classified according to their physical state and chemical composition.
Due to their high altitude and the curvature of the surface of the Earth, these clouds will receive sunlight from below the horizon and reflect it to the ground, shining brightly well before dawn or after dusk.
PSCs form at very low temperatures, below −78 °C (−108 °F). These temperatures can occur in the lower stratosphere in polar winter. In the Antarctic, temperatures below −88 °C (−126 °F) frequently cause type II PSCs. Such low temperatures are rarer in the Arctic. In the Northern hemisphere, the generation of lee waves by mountains may locally cool the lower stratosphere and lead to the formation of PSCs.
Forward-scattering of sunlight within the clouds produces a pearly-white appearance. Particles within the optically thin clouds cause colored Interference fringes by diffraction. The visibility of the colors may be enhanced with a polarising filter.
Types
PSCs are classified into three types Ia, Ib and II according to their chemical composition which can be measured using LIDAR. The technique also determines the height and ambient temperature of the cloud.
Only Type II clouds are necessarily nacreous whereas Type I clouds can be iridescent under certain conditions, just as any other cloud.