Atmokinesis

Cloud Formation

	by Theresa M. Kelly, MsD
	Professor of Scientific Parapsychology, Researcher, Technical Author

Atmokinesis is the psychical influence of meteorological phenomena including the states of the atmosphere as measured on temperature, humidity, clarity, and activity scales. Experient influenced meteorological phenomena (weather events) are limited to current or predicted events occurring in the troposphere, which is the lowest portion of Earth’s atmosphere.

A cloud is a visible mass of small water droplets or frozen water crystals (0.01 mm diameter) suspended in the atmosphere above the surface of the Earth. Denser clouds appear white because they exhibit a high reflectance (70% to 95%) throughout the visible wavelengths, at least from the top.

In exercises pertaining to cloud formation, experients direct and concentrate large masses of humidity (water vapor) into a small area above them and then cool the area within the concentration just enough to cause cloud formation without initiating precipitation by avoiding temperatures at or below the dew point.

The most commonly reported clouds formed by experients are Family C clouds (mainly cumulus and stratus clouds) and when these clouds contact the ground, they are called fog. Cumulus clouds are often referred to as “puffy” or “cotton-like” in appearance. These clouds may appear alone, in lines, or in clusters.

Stratus clouds are characterized bas clouds horizontally layering the sky with a uniform base, as opposed to convective clouds, which are tall or taller than they are wide (cumulus). These clouds can be described as flat, hazy, featureless clouds of low altitude varying from dark gray to nearly white.

Source

(Adapted from the paper “ Manual of Atmokinesis: Applications, Experimentation, and Measurement ” by Theresa M. Kelly, MsD.)

Related Articles

• Atmokinesis: Misconceptions and Myth - Associated Limits and Dangers
• Atmokinesis: Influence Takes Time – Minutes, Hours, Days
• Atmokinesis: Chaotic Systems and Prediction Limitation
• Atmokinesis: Spontaneous Heating and Cooling
• Atmokinesis: Prevailing Winds and Forms of Measurement