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The density of accreted ice

✍ Scribed by F. Prodi; L. Levi; P. Pederzoli

Publisher
John Wiley and Sons
Year
1986
Tongue
English
Weight
694 KB
Volume
112
Category
Article
ISSN
0035-9009

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πŸ“œ SIMILAR VOLUMES

Comments on β€˜The density of natural ice
Comments on β€˜The density of natural ice accretions related to non-dimensional icing parameters’ by K. F. Jones (January B 1990, 116, 477-496)
✍ L. Levi; F. Prodi πŸ“‚ Article πŸ“… 1993 πŸ› John Wiley and Sons 🌐 English βš– 382 KB

## Abstract The results obtained by applying the various equations relating the accreted ice density, __p__, to the growth parameters are compared with each other and with direct experimental results. Special attention is paid to the equation recently proposed by Jones, in which, taking into accoun

Reply to comments by L. Levi and F. Prod
Reply to comments by L. Levi and F. Prodi: Another look at the dependence of ice accretion density on non-dimensional parameters
✍ Kathleen F. Jones πŸ“‚ Article πŸ“… 1993 πŸ› John Wiley and Sons 🌐 English βš– 322 KB

## Abstract In response to the comments of Levi and Prodi I have made a comparison between their rime density data and a similar subset of my data. The choice of air temperature rather than accretion temperature to characterize droplet freezing is further explained, and the convective‐heat‐flux π‐p

The opacity of accreted ice
The opacity of accreted ice
✍ J. N. Carras; W. C. Macklin πŸ“‚ Article πŸ“… 1975 πŸ› John Wiley and Sons 🌐 English βš– 221 KB

## Abstract A technique which yields quantitative measurements of the opacity of accreted ice deposits is described. This consists of determining the attenuation of a light beam as it passes through a thin section of the deposit, using a photovoltaic cell as the detector. The transmittance of the d

Three-dimensional modelling of ice accre
Three-dimensional modelling of ice accretion density
✍ Krzysztof Szilder; Edward P. Lozowski πŸ“‚ Article πŸ“… 2000 πŸ› John Wiley and Sons 🌐 English βš– 638 KB

## Abstract A three‐dimensional, random‐walk, ballistic model is used to simulate the density and structure of an ice accretion formed by impinging supercooled droplets. The model is calibrated using experimental observations of the ice density at the stagnation line on a fixed circular cylinder. A