Analysis of the global spectrum of the atmospheric horizontal kinetic energy from the boundary layer to the mesopause
Brune, Sebastian
1974-
aut
text
theses
Text
Hochschulschrift
gw
2012
monographic
XA-DE
2012
eng
text/html
application/pdf
Online-Ressource graph. Darst.
This thesis contributes to the discussion, how the large-scale and mesoscale atmospheric motions interact and how the vertical coupling of the atmosphere is influenced by mesoscale waves. The results from our mechanistic GCM are twofold. Firstly, the mesoscale upper tropospheric kinetic energy spectrum can be explained by stratified turbulence. Secondly, the mesoscale energy deposition in the upper mesosphere can be explained by the vertical pressure flux carried by mesoscale gravity waves from the troposphere, which is converted into kinetic energy of these waves and then dissipated.
vorgelegt von: Sebastian Brune
Rostock, Univ., Mathematisch-Naturwiss. Fak., Diss., 2012
UT 5100
38.81
http://rosdok.uni-rostock.de/resolve?urn=urn:nbn:de:gbv:28-diss2012-0082-2
http://rosdok.uni-rostock.de/resolve?urn=urn:nbn:de:gbv:28-diss2012-0082-2&pdf
http://nbn-resolving.de/urn:nbn:de:gbv:28-diss2012-0082-2
Analysis of the global spectrum of the atmospheric horizontal kinetic energy from the boundary layer to the mesopause
2012
Druck-Ausgabe
(DE-627)716340194
Brune, Sebastian, 1974 -
urn:nbn:de:gbv:28-diss2012-0082-2
934850524
rakwb
DE-627
121025
728562693
20240716T200543.0
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