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The isotopic analysis of hailstones

โœ Scribed by W. C. Macklin; M. Majoube; L. Merlivat


Publisher
John Wiley and Sons
Year
1972
Tongue
English
Weight
96 KB
Volume
98
Category
Article
ISSN
0035-9009

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๐Ÿ“œ SIMILAR VOLUMES


The fallspeeds of hailstones
โœ W. C. Macklin; F. H. Ludlam ๐Ÿ“‚ Article ๐Ÿ“… 1961 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 539 KB

## Abstract Measurements have been made of the speeds of ice objects resembling hailstones during free fall, and of the drag coefficients of such objects and of natural hailstones. It has been found that the drag coefficients range from those of spheres (about 0ยท45) to about 0ยท8, depending on the s

The fallspeeds of hailstones
โœ W. C. Macklin; F. H. Ludlam ๐Ÿ“‚ Article ๐Ÿ“… 1961 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 171 KB
The collection efficiencies of hailstone
โœ W. C. Macklin; I. H. Bailey ๐Ÿ“‚ Article ๐Ÿ“… 1968 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 256 KB
The aerodynamics of oblate hailstones
โœ S. Thwaites; J. N. Carras; W. C. McKlin ๐Ÿ“‚ Article ๐Ÿ“… 1977 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 523 KB

## Abstract Artifical hailstones having shapes and structures closely resembling natural oblate hailstones have been grown in a vertical icing tunnel. These hailstones were grown by spinning them about the minor axis and at the same time causing the minor axis to move in a conical manner about the

On the melting of hailstones
โœ B. J. Mason ๐Ÿ“‚ Article ๐Ÿ“… 1956 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 410 KB

## Abstract Calculations have been made on the rate of melting of solid ice spheres and of graupel particles as they fall from the 0ยฐC level towards the ground. Graphs are drawn for particles of various initial radii showing the radius of the unmelted core as a function of the distance fallen, and

The density and structure of hailstones
โœ K. A. Browning; F. H. Ludlam; W. C. Macklin ๐Ÿ“‚ Article ๐Ÿ“… 1963 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 738 KB

## Abstract Macklin's (1962) experimental study of ice accretions, together with estimates of the typical conditions in the cumulonimbus of cold air masses and of summer continental air masses, is used to deduce the density of ice in the hailstones produced by these clouds. It is shown that general