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JUST like
the tsunami has been known to be destructive but never taken
seriously to warrant the installation of early warning systems
in the Indian Ocean, thunderstorms and hailstorms have never
been taken seriously either by the authorities in Africa’s
Great Lakes region in general and the areas around Lake Victoria
in particular.
Tsunami is a Japanese word, which means tidal waves. They are
known as harbours’ tides because they move horizontally
along the seabed and only rise vertically as they hit the shoreline,
unlike the conventional common sea tide waves that are seen
on the surface.
This characteristic of tsunami was one of the main causes of
death to people who had rushed to the seashore to find out why
the water had rapidly receded many metres, only to be caught
unawares by returning waves that had risen again several metres
as they approached the shoreline at very high speeds.
It was a sheer act of God for survivors to have managed to be
thrown to safer grounds. Year after year, hailstorms have caused
havoc to crops and other properties in the Great Lakes region.
Had statistics been correctly gathered and kept by the relevant
authorities, the red flags would have been rising to attract
remedial action.
Like in the tsunami case, some of the hailstorms will be larger
and more destructive. Sometimes they comprise large hailstones,
and some have been reported to be as large as an elephant, while
others are merely 25 feet in diameter.
However, the largest hailstorm reported by Weather Bureau officials
was one that fell at Potter, Nebraska, US which reportedly killed
people. In northern India in 1888, hailstones as large as cricket
balls killed 246 people as well as 1,600 sheep and goats.
Another storm in Western Hunan province of China killed 200
people and injured thousands in 1932.
On May 13, 1939, at Lubbock, Texas, a farmer died of injuries
when he was caught in an open field during a severe hailstorm.
The World Food Programme (WFP) and Care International have been
providing some early warning information to the Kenya government
through the vulnerability analysis and mapping (VAM) programme.
But the warnings have been downplayed although their lethal
results are known.
One of the surprises of a hot afternoon thunderstorm is the
almost magical transformation of the landscape from green icy
white with the onset of a hailstorm. Hailstorms may occur if
convective activity and sufficient moisture are present and
if the freezing level in the skies is relatively low.
The first sign that a hailstorm may be coming is growing whitening
among the shafts of rain. A hail shaft is a column of ball falling
from a single thunderstorm cell. The ground area swept by the
hail shaft is known as a hail streak, which is typically produced
by a hail cell moving along at 30-45 miles per hour, although
speeds of 60 miles per hour have been recorded.
Hail streaks, which are highly mobile, cover areas varying from
100 feet to 2 miles wide and about 5 miles long. A hailstorm
can be the most damaging part of a thunderstorm, inflicting
injury on humans and animals and destroying crops and property.
The writer is a retired civil servant.
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