Polar Stratospheric Cloud Alert At top right is the twilight scene of vivid reds imaged by Pete Glastonbury at Devizes in Wiltshire, England. Polar Stratospheric Clouds, PSCs, occur at heights of 15-25 km (9-16 mile) and far above our ordinary tropospheric clouds. To form in the arid and low density conditions of the lower stratosphere they need temperatures of minus 78�C or colder depending on their composition. Type I PSCs are nitrogen acid and water compounds. Type 2, the brightly shining nacreous clouds, are ice and they need slightly lower temperatures. A large part of Europe had similar spectacular sunsets and twilights in February 2008 caused by very low stratospheric temperatures and Type I PSCs (see the thumbnail links below). Volcanic aerosol and dust give similar sunsets and we should not rule out these possibilities at this stage. We could be seeing the start of a series of spectacular sunsets. Look out for twilights and sunrise/sets over the next few days. |
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