Abstract
Abstract. 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.
References
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Referenced
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Dates
Type | When |
---|---|
Created | 15 years, 3 months ago (April 29, 2010, 10:09 a.m.) |
Deposited | 4 years, 6 months ago (Jan. 29, 2021, 8:43 p.m.) |
Indexed | 3 months ago (May 16, 2025, 4:06 a.m.) |
Issued | 16 years, 6 months ago (Jan. 28, 2009) |
Published | 16 years, 6 months ago (Jan. 28, 2009) |
Published Online | 16 years, 6 months ago (Jan. 28, 2009) |
@article{Spichtinger_2009, title={Modelling of cirrus clouds – Part 1b: Structuring cirrus clouds by dynamics}, volume={9}, ISSN={1680-7324}, url={http://dx.doi.org/10.5194/acp-9-707-2009}, DOI={10.5194/acp-9-707-2009}, number={2}, journal={Atmospheric Chemistry and Physics}, publisher={Copernicus GmbH}, author={Spichtinger, P. and Gierens, K. M.}, year={2009}, month=jan, pages={707–719} }