For nearly two thousand years, the ancient Greek philosopher Aristotle (384-322 BCE) dominated the subject of meteorology. According to Aristotle, weather resulted from the cyclical movement of two exhalations: one hot and dry like fire, the other vaporous and water-like. When heat from the sun caused water to break into smaller parts, vapour rose into the upper regions of the air whereas cold exhalations caused the vapour to fall back to the earth.
Aristotelian vapour theory persisted in seventeenth- and eighteenth-century notions of meteorological phenomena. Following this tradition, natural philosophers believed that the earth exhaled flammable vapours that would ignite in the atmosphere as lightning or aurora borealis, for instance. Sulphuric or nitric in nature, it was also believed that these fumes sometimes ignited underground causing earthquakes.
For individuals who supported Aristotelian-based theories of earthly exhalations, instruments used to measure the physical qualities of air - such as weight, temperature and water-vapour content - did not play a significant role for studying meteorological phenomena. Instead, they often employed analogies of gunpowder to model and understand how nature produced lightning sparks or glowing skies.