000014520 001__ 14520
000014520 005__ 20161115100154.0
000014520 04107 $$aeng
000014520 046__ $$k2016-08-21
000014520 100__ $$aShaw, Raymond
000014520 24500 $$aCloud formation through isobaric mixing in turbulent Rayleigh- Bénard convection

000014520 24630 $$n24.$$p24th International Congress of Theoretical and Applied Mechanics - Book of Papers
000014520 260__ $$bInternational Union of Theoretical and Applied Mechanics, 2016
000014520 506__ $$arestricted
000014520 520__ $$2eng$$aCloud formation through isobaric mixing of water vapor in turbulent Rayleigh-B´enard convection is studied in the Michigan Tech Pi Chamber (aspect ratio, diameter over height, of 2). Steady-state cloud conditions are achieved, allowing reliable sampling of turbulent time series of air velocity, temperature, water vapor concentration, and cloud droplet size distribution. The water vapor and temperature measurements allow for quantification of the turbulent fluctuations of water vapor supersaturation. For large temperature differences (high Rayleigh number), the droplet size distributions exhibit a pronounced large-drop tail reminiscent of drizzle formation. This opens the door for controlled, laboratory studies of aerosol-cloud-drizzle interactions.

000014520 540__ $$aText je chráněný podle autorského zákona č. 121/2000 Sb.
000014520 653__ $$a

000014520 7112_ $$a24th International Congress of Theoretical and Applied Mechanics$$cMontreal (CA)$$d2016-08-21 / 2016-08-26$$gICTAM2016
000014520 720__ $$aShaw, Raymond
000014520 8560_ $$ffischerc@itam.cas.cz
000014520 8564_ $$s343861$$uhttps://invenio.itam.cas.cz/record/14520/files/TS.FM05-4.03.pdf$$yOriginal version of the author's contribution as presented on CD,  page 743, code TS.FM05-4.03
.
000014520 962__ $$r13812
000014520 980__ $$aPAPER