Modelling of cirrus clouds – Part 1b: Structuring cirrus clouds by dynamics

A recently developed and validated bulk microphysics scheme for modelling cirrus clouds (Spichtinger and Gierens, 2009), implemented into the anelastic non-hydrostatic model EULAG is used for investigation of the impact of dynamics on the evolution of an arctic cirrostratus. Sensitivity studies are...

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Bibliographic Details
Published in:Atmospheric Chemistry and Physics
Main Authors: Spichtinger, P., Gierens, K. M.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2009
Subjects:
Online Access:https://doi.org/10.5194/acp-9-707-2009
https://noa.gwlb.de/receive/cop_mods_00047896
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00047516/acp-9-707-2009.pdf
https://acp.copernicus.org/articles/9/707/2009/acp-9-707-2009.pdf
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Summary:A recently developed and validated bulk microphysics scheme for modelling cirrus clouds (Spichtinger and Gierens, 2009), implemented into the anelastic non-hydrostatic model EULAG is used for investigation of the impact of dynamics on the evolution of an arctic cirrostratus. Sensitivity studies are performed, using variation of large-scale updraughts as well as addition of small-scale temperature fluctuations and wind shear. The results show the importance of sedimentation of ice crystals on cloud evolution. Due to non-linear processes like homogeneous nucleation situations can arise where small changes in the outer parameters have large effects on the resulting cloud structure. In-cloud ice supersaturation is a common feature of all our simulations, and we show that dynamics is as least as important for its appearance than is microphysics.