1. Ice Supersaturation Variability in Cirrus Clouds: Role of Vertical Wind Speeds and Deposition Coefficients.
- Author
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Kärcher, B., Jensen, E. J., Pokrifka, G. F., and Harrington, J. Y.
- Subjects
CIRRUS clouds ,WIND speed ,SUPERSATURATION ,ICE crystals ,ICE prevention & control - Abstract
Aircraft measurements reveal ice supersaturation statistics in cirrus (ISSs) with broad maxima around ice saturation and pronounced variance. In this study, processes shaping ISSs in midlatitude and tropical upper tropospheric conditions are systematically investigated. Water vapor deposition and sublimation of size‐resolved ice crystal populations are simulated in an air parcel framework. Mesoscale temperature fluctuations (MTFs) due to gravity waves force the temporal evolution of supersaturation. Various levels of background wave forcing and cirrus thickness are distinguished in stochastic ensemble simulations. Kinetic limitations to ice mass growth are brought about by supersaturation‐dependent deposition coefficients that represent efficient and inefficient growth modes as a function of ice crystal size. The simulations identify a wide range of deposition coefficients in cirrus, but most values stay above 0.01 such that kinetic limitations to water uptake remain moderate. Supersaturation quenching times are long, typically 0.5–2 hr. The wave forcing thus causes a remarkably large variability in ISSs and cirrus microphysical properties except in the thickest cirrus, producing ensemble‐mean ISSs in line with in‐situ measurements. ISS variance is controlled by MTFs and increases with decreasing cirrus integral radii. In comparison, the impact of ice crystal growth rates on ISSs is small. These results contribute to efforts directed at identifying and solving issues associated with ice‐supersaturated areas and non‐equilibrium cirrus physics in global models. Plain Language Summary: Measurements show that cold, high cirrus clouds evolve in ice‐supersaturated states away from equilibrium, which sets them apart from low‐level liquid water clouds. Such cloud states are brought about by rapidly displacing cloudy air parcels in the vertical wind field. The resulting temperature changes cause ice crystals to either grow or shrink in size by uptake or release of water molecules, which, in turn, tends to restore equilibrium. We carefully examine how ice supersaturation and cirrus properties respond to changes in vertical wind speeds for various ice growth models. We show that cloud‐scale wave motions determine to a large extent the frequency of occurrence of ice‐supersaturated states. The sensitivity to cloud ice growth is much weaker. Our results help interpret atmospheric observations and may improve the representation of cirrus in global models. Key Points: This study presents a process‐based, systematic investigation of key factors controlling ice supersaturation statistics within cirrusGravity wave‐induced mesoscale temperature fluctuations cause a remarkably large variability in ice supersaturationIce supersaturation statistics are not strongly modified by depositional growth with supersaturation‐dependent deposition coefficients [ABSTRACT FROM AUTHOR]
- Published
- 2023
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