|
Hail facts
Biggest
hail stone: A hailstone measuring 8 inches in diameter and weighing
1.67 pounds, was found in Coffeyville, Kansas on 3rd September 1970.
The largest
hailstone on record to fall in the United States was in Coffeyville
on Sept. 3, 1970. It measured 7.5 inches in diameter and weighed
1.67 pounds.
Hailstones
form in the updraft of a thunderstorm with stronger storms producing
larger hail. The updrafts pull the precipitation up into the cloud,
adding layer upon layer of moisture.
Cut in half,
a hailstone has concentric rings like an onion, which reveals the
number of times it traveled to the top of the storm before falling
to Earth.
A thunderstorm
is classified as severe when hailstones are three-fourths of an
inch or larger and winds exceed 58 mph.
Hailstones
can range from pea-sized (one-quarter inch) to golfball-sized (1.75
inches) to softball-sized (4.50 inches.)
While rarely
a threat to physical safety, large hail results in nearly $1 billion
a year in damage to property such as crops, roofs, automobiles and
other outdoor objects.
When the hail
falls to Earth, they come zipping down at 70 to 100 mph. That is
why it is a good idea to stay indoors during a major hailstorm!
Source: FEMA, National Weather Service.
Hail Facts
about Colorado
The hail season in Colorado is March through October.
June has the highest frequency statewide, averaging over 130 reported
severe hailstorms a year.
The vast majority of hail occurs May through August.
Fort Collins has its most frequent hailstorms in May, but its largest
hail comes in July and August.
Hail is primarily an afternoon or evening phenomenon in Colorado.
Most severe hailstorms occur between 1:00 p.m. and 9:00 p.m. MST.
Hailstorms rarely last more than 15 minutes at any given location.
The median duration is 6 minutes.
The storm itself may drop hail continuously for several hours along
its path.
In Colorado, hail is a regional problem.
It rarely hails in the mountains or on the Western Slope.
Hail severity increases as you go east from the Front Range foothills
toward the Kansas border.
Source - Nolan Doesken, Colorado Climate Center
|