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(Dated: September 12, 2007)

I. Introduction (Times New Roman 10-bold centre justified capital)

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The problem of hail formation and hail forecasting had been faced by several authors (Fawbush and Miller, 1953; Ludlam, 1958; Prodi and Wirth, 1973; Morgan, 1973), nevertheless, even if the general understanding of this phenomenon is highly increased, it still presents some open questions mainly because its occurrence involves both mesoscale and microphysical processes ...

II. Presentation of Research (Times New Roman 10-bold centre justified capital)

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The effects of mixing ratio on hailstone growth are analyzed using a simple analytical model where it is assumed that the growth process is entirely due to the collection of supercooled droplets. With this assumption, the growth equation becomes (Mason, 1971; Knight and Knight, 2001)

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III. Results and Conclusions (Times New Roman 10-bold centre justified capital )

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In this, work it is shown that the average mixing ratio vertical profile over the Friuli Venezia Giulia plain is not constant, neither in the various months of the year nor in the four times-of-the-day. In particular, the amount of mixing ratio increases from January to August and from morning (06 UTC) to night (00 UTC), being the last differences particularly evident in July, August and September.

Taking into account these differences and using a simple analytical model for hail growth, it has been possible to reproduce the order of magnitude of the observed differences in the shape of the hailstone size distribution in the four times-of-the-day...

IV. Aknowledgments

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The authors would like to thank all the volunteers who, since 1988, contribute to the collection of the hailpads. Without their effort, this work ...

V. References

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Giaiotti D. B., Stel F., 2006: Environmental Variables Affecting the Hailstone Size Distribution at the Ground. Atmos. Res., 20 109-112.

4th European Conference on Severe Storms 10 - 14 September 2007 - Trieste - ITALY

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stel

2006-11-26T21:39:00

Dario Giaiotti