3-D modeling of noctilucent cloud evolution and relationship to the ambient atmosphere
Kiliani, Johannes
1981-
aut
text
theses
Text
Hochschulschrift
gw
2014
monographic
XA-DE
2014
eng
text/html
application/pdf
Online-Ressource Ill., graph. Darst.
Noctilucent clouds (NLC) at the polar summer mesosphere are highly sensitive to atmospheric conditions, therefore they are an important climate indicator. In this thesis, an ice particle model is combined with circulation models to simulate the formation of NLC throughout the particle life cycle: Only 1% of ice particles grow to visible size (50 nm). The main part of particle growth takes place at 83 km altitude, within 6 hours prior to observation and is accompanied by upwelling. By using cylindrical particle shape, the simulated optical signal is made consistent with measurements.
von Johannes Kiliani
Rostock, Univ., Diss., 2014
551.567
550
UT 5250
38.81
http://rosdok.uni-rostock.de/resolve?urn=urn:nbn:de:gbv:28-diss2015-0028-8
http://rosdok.uni-rostock.de/resolve?urn=urn:nbn:de:gbv:28-diss2015-0028-8&pdf
http://nbn-resolving.de/urn:nbn:de:gbv:28-diss2015-0028-8
3-D modeling of noctilucent cloud evolution and relationship to the ambient atmosphere
Kühlungsborn : IAP, 2014
Druck-Ausgabe
(DE-627)812861019
Kiliani, Johannes, 1981 -
urn:nbn:de:gbv:28-diss2015-0028-8
935808480
rakwb
DE-627
150212
817983767
20251224T194950.0
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