# Hail stones in summer?

This has always puzzled me. Yesterday (in London) it started hailing despite it being about $20^oC$. A couple of years ago I experienced hail in Sicily when it was about $35^oC$ in the shade!. How is this possible?

-
Sorry, but your Question at least does not show as much research effort as would be required to Google for hail and go to en.wikipedia.org/wiki/Hail. There are interesting details, but basically it's colder at altitude. –  Peter Morgan Jun 24 '11 at 12:07
I feel some nice answer may appear, so I'll let it stay for now -- this is way more complex than colder at altitude; in fact large temperature near the ground helps. –  mbq Jun 24 '11 at 16:46
add comment

## 1 Answer

Temperature generally gets cooler as you go higher in altitude (which is one reason why you have snow on mountain peaks long after it has melted away in the foothills).

Hail develops in thunderstorms. A thunderstorm ~BY DEFINITION~ is a storm which has developed through the freezing layer. So think about this: If you see lightning or hear thunder from a storm, you can be absolutely sure that at least part of that storm is above the freezing altitude, and at least part of the storm is below it. Thunderstorms often develop on warm days; and they also often develop on the edge of a cold front, where cold air is overtaking and riding over the less dense warmer air.

A typical thunderstorm case: It is a very warm day, and the air might be quite humid. The warm moist air tries to rise to get higher than the cooler drier (and therefore heavier) air above it. The moist air rises. As it rises it cools past its dew point and moisture droplets precipitate. These droplets can be blown up by the rising air, higher than the freezing altitude, where they freeze. They start falling through the moist air, freezing a layer of moisture onto the small iceball, then may be blown up again by updrafts. The process can repeat many times as the little iceball goes up and down past the freezing level, each time growing by adding another layer of frozen moisture.

Eventually the little iceball is too heavy for the updrafts to keep it aloft in the freezing zone, and it falls to earth as hail.

-
Very nice description. Standing at the base of Popocatepet "Its a 18,000 ft volcano close to Mexico Ct." you can actually see this happen. You see the humidity rise from one valley the frozen jet-stream coming of the volcano will carry it to the next sunny valley where you get bearing like hail. This kind of hail is very hard ice and comes down fast. We had to describe the phenomena as part of geo-physics class –  Fortunato Jun 26 '11 at 8:07
add comment