Noctilucent cloud

Noctilucent clouds (also known as polar mesospheric clouds) are rare bright cloudlike atmospheric phenomena visible in a deep twilight (the name means roughly "night shining"). They are most commonly observed in the summer months at latitudes between 50° and 60° (north and south).

They are the highest clouds in the Earth's atmosphere, being located in the mesosphere at altitudes of around 85km, and are visible only when illuminated by sunlight from below the horizon while the ground and lower layers of the atmosphere are in the Earth's shadow; otherwise they are too faint to be seen.

Noctilucent clouds are not fully understood. It was once proposed that they were composed of volcanic or meteoric dust, but they are now known to be primarily composed of water ice (confirmed by UARS). They appear to be a relatively recent phenomenon--they were first reported in 1885, shortly after the eruption of Krakatoa--and it has been suggested that they may be related to climate change.

They are studied from the ground, from space, and in situ by sounding rockets; they are too high to be reached by balloons. The AIM satellite mission, scheduled for launch in 2006, is dedicated to research into noctilucent clouds.

See also

• Nacreous clouds
• Polar stratospheric clouds

External links

• AIM satellite mission: http://aim.hamptonu.edu/
• Gary Thomas's page at U. Colorado: http://lasp.colorado.edu/noctilucent_clouds/
• http://www.nlcnet.co.uk/
• http://www.meteo.helsinki.fi/~tpnousia/nlcgal/nlcgal.html
• http://gwest.gats-inc.com/nlc_cam.php