Summary

Jacques Wardlaw Redway Handbook of Meteorology — The Atmosphere and Its Constituents (1921)

Meteorology is the science of the air. The air is the outer shell, or layer, of the earth; hence it is called the atmosphere, a Greek word meaning “air-sphere”. The movements of the air (the winds) and the variable proportion of water vapor, mingled with and forming a part of it, exert a profound influence which affects the climate, habitability and civilization of the earth.
For the greater part the movements of the air and the variations in the proportion of moisture are the results of changes in temperature.
Source: Wikisource

Jacques Wardlaw Redway Handbook of Meteorology — The Atmosphere and Its Constituents (1921)

The floating dust motes of the air are factors of great meteorological importance. They are the nuclei upon which the water vapor of the air condenses. Dense clouds of volcanic dust act as a screen preventing much of the sun’s heat from reaching the earth. The dust particle is the normal nucleus for the cloud particle. The flying, or windblown dust, though a highly important physiographic agent, is not a factor of importance in meteorology.
Source: Wikisource

Jacques Wardlaw Redway Handbook of Meteorology — The Atmosphere and Its Constituents (1921)

Dust particles so fine that they escape measurement even with the highest power of the microscope, must be considered a part of the normal content of the atmosphere. Their presence is indicated by the fact that they may reflect enough light to make them visible en masse when a powerful light is turned upon them in a darkened room, or when a searchlight throws its beam at night. The path of the light is shown by the light reflected from dust motes. Dust particles of the size thus revealed behave like molecular rather than like matter of molar sizes.
Source: Wikisource

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