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100
In a recent interview , Richards explained the super-transistor effect
which others also describe as an avalanche of electrons. At certain frequencies and at a
certain energetic threshold, there is a large energy transfer between levels in the
upper atmosphere.
EFFECTS REACH THE GROUND
How far down from the magnetosphere or ionosphere through the
atmosphere can such an "avalanche" come? Surprisingly, in various locations
Richards found effects reaching the earth. The first time he saw this recorded on
scientific instruments, he was living at 8,000 feet above sea level in central-west
New Mexico where the air was clear and electromagnetically quiet. That day there
was
a large buildup of electrical energy in the atmosphere very close to the surface of the
earth, but not a thunderstorm condition. As the non-lightning electrical condition
passed through the area, Richards and his associates monitored surprisingly large
oscillations (vibrations) on their antennae array and learned at what frequencies the
local atmosphere readily vibrates. The vibrations charged capacitors (energy storage
units) to a rather high voltage.
One quiet March day while monitoring the Russian and American ELF
transmissions, they tried running an antenna array (twisted wires) a mile along the
ground, and received unexpectedly strong and continuous signals. Briefly, the
findings and further monitoring were a springboard for discovering correlations with
harmonic interactions between the planets. They also learned how nature handles the
influx of cosmic energy towards earth's surface through the auroral vibrations. The
researchers saw how energies could be stored within the magnetosphere, and "we
have a mechanism, confirming Tesla, for drawing this energy into the lower
atmospheric cavity."
'COUPLING' BETWEEN IONOSPHERE AND WEATHER
While Richards' interest in their work was to find a usable clean- energy
source for the inhabitants of Earth, physicists at Stanford University worked on a
government funded project. They wanted to amplify waves in the magnetosphere for
the goal of global communication at lower frequencies.101
The authors of this book have a different aim - to understand the ramifications of the
high-level experiments. Could it affect our weather? The atmospheric physicists we
have spoken to are vague in their answers.
The paper by Richards gives strong clues. Recent scientific evidence
suggests that strong electrical coupling exists between the ionosphere and lower
atmosphere, he said. Large scale horizontal electric fields move down from the
magnetosphere and ionosphere, with little loss of amplitude, to around ten
kilometers above the earth, he said, "The total potential voltage drop across regions
like the polar caps and the auroral ionosphere can be a significant fraction of the
average ionospheric potential with respect to the earth..."
100 E.E. Richards, conversation with Jeane Manning, May 1995,
101 "VLF: Getting Panicles Excited," Science News, Dec, 18 and 25, 1982, pg. 392.