Summary

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.
Source: Wikisource

Hugh Robert Mill Encyclopædia Britannica, Ninth Edition (1888)

To ensure perfect uniformity in registration, the bulbs should all be as nearly as possible of one size, constructed of one kind of glass, and the mounting perfectly uniform. Better-class instruments have the bulb clear of the frame, and the stem attached to a slab of metal, of porcelain, or of glass backed by wood; but sometimes they are simply fixed to a boxwood scale. In all cases they should he graduated on the stem, and compared with a standard, but in view of the uncertainty of the methods of thermometer exposure great delicacy is undesirable.
Source: Wikisource

Hugh Robert Mill Encyclopædia Britannica, Ninth Edition (1888)

In meteorology radiation is measured by thermometers simply exposed with blackened bulbs. Results of the utmost diversity are given by different methods. As there is no means of determining the true measure of radiation, all that can be done is to have the instruments whose indications are to be compared constructed and exposed in the same way. The usual form, as suggested by Herschel, is a maximum thermometer with a spherical bulb half an inch in diameter coated with lamp-black and placed in the centre of a spherical vessel of clear glass, 21/2 inches in diameter, and exhausted of air.
Source: Wikisource

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