Hugh Robert Mill, Encyclopædia Britannica, Ninth Edition (1888)
“ Fahrenheit’s scale is convenient for meteorological work on account of its short degrees, admitting of great accuracy in reading and compactness in recording, and on account of its low zero, which makes it possible in temperate climates to dispense with negative quantities. On the other hand, the centigrade scale is on the whole so convenient, its use is so nearly universal, and the advantage of a uniform system is so great that it must ultimately be adopted for all purposes. [1] Air Thermometer.—Under constant pressure gases expand equally for equal increments of heat. ”
