OLLIVIER HAIL SUPPRESSION SYSTEM
The ascending currents (in red) and descending (in blue) undergo repetitiously the disturbances generated by the 2 ton thrust of the elliptic shockwave emitted by the accelerator of the positive ionic particies (the Olliver System®) provoking by electrolysis the unstabilizing of the ice molecules. This ionic bombardment permits to desolve the hail that's falling in to a fine rainfail in the zone protected by the system 100 hectares (250 acres).
A
thunderstorm
is the most impressive manifestation of atmospheric electricity. The
onization of the atmosphere and the condensation of water vapor on the
ions changes water vapor into negatively charged liquid droplets when
reaching an altitude of
1000
m (3,300 ft) or 2 000 m (6,500 ft). Water droplets in a cloud are kept
apart by their repulsive electrical force. This repulsion is at the
origin of the internal equilibrium of the cloud, creating a true
suspension of water in the Acetylene is a highly explosive gas. The
speed of the elliptical funnel-shaped shock waves is a direct
consequence of the detonation that takes place in a very precise part of
the system. The set of emitted and reflected waves affects the clouds'
microstructure avoiding thus the crystallization of the water droplets
in suspension.
The
efficiency of the system is based on the multiplication, every 6
seconds, of 2 tons of positively ionized shock waves. The ionized shock
waves fulfill their role as provokers of microstructural instability
inside the cumulonimbus. The dynamics of a thunderstorm are often more
complex than described above. Our fifteen years of experience in the
field have shown us that protection is increased through the use of
several HSE Hail Suppression Systems@ functioningO in group formation.
Highly speciflc, low-frequency sound waves can be used to destabilize
certain values and conditions that allow cumulonimbus to evolve. The
steady firing of HSE Hail Suppression System@ produces an accumulation
of shock waves and sonic vibrations in the atmosphere and forms a
cushion between the base of the cloud and the ground.
To ensure maximum efficiency, the HSE Hail
Suppression System@ must begin its operation while the storms are still
in the development stage, 7 minutes before the cloud formation is
directly above the protected area. This allows the shock waves to reach
their maximum intensity over a 3 Km (2 mi.) diameter area, at an
altitude of 8000 m (26,000 ft) to 15 000 m (50,000 ff) and more.
We
also propose the use
of a radar to detect and analyze clouds, as well as to automatically
trigger the HSE Hail Suppression System@. This increases the system's
reliability by eliminating human intervention and error.
To summarize, the HSE Hail Suppression System@
offers a leading-edge technology that eliminates hailstone damage in the
area protected by the shock waves. Although snowflakes may fall in the
protected zone, the system does not diminish rainfall in any way. The
system is also very efficient against freezing ram.