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scostep 2010 (stp12) - Leibniz-Institut für Atmosphärenphysik an der ...

scostep 2010 (stp12) - Leibniz-Institut für Atmosphärenphysik an der ...

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STP12 Abstracts<br />

Berlin, 12 - 16 July <strong>2010</strong><br />

SCOSTEP Symposium <strong>2010</strong><br />

The Role of Meteoric Smoke Particles in the Polar Middle Atmosphere<br />

Rapp Markus<br />

<strong>Leibniz</strong>-<strong>Institut</strong>e of Atmospheric Physics at the Rostock University, Kühlungsborn, Germ<strong>an</strong>y<br />

Meteoric smoke particles (MSPs) are thought to be formed as secondary meteoroid ablation<br />

products when part of the meteoric material deposited in the altitude r<strong>an</strong>ge from 70 - 100 km<br />

recondenses to form n<strong>an</strong>ometer-scale particles which may then further develop by coagulation<br />

<strong>an</strong>d tr<strong>an</strong>sport. It is current belief that MSPs play <strong>an</strong> import<strong>an</strong>t role in several middle<br />

atmosphere phenomena such as the nucleation of mesospheric ice clouds, the metal layers, the<br />

tr<strong>an</strong>sport of meteoric material to the ground, <strong>an</strong>d even the formation of polar stratospheric<br />

clouds which in turn play a signific<strong>an</strong>t role in the context of ozone destruction during polar<br />

spring. While MSPs have long been deemed import<strong>an</strong>t for all these processes, solid<br />

experimental results on their properties have only recently been acquired with the availability<br />

of new rocket-, radar- <strong>an</strong>d satellite-techniques. This paper reviews our current knowledge<br />

regarding MSPs taking into account all these new experimental sources as well as recent<br />

model results <strong>an</strong>d closes with suggestions for future work.

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