Quick Facts
Born:
November 27, 1701, Uppsala, Sweden
Died:
April 25, 1744, Uppsala (aged 42)
Inventions:
Celsius
Subjects Of Study:
northern lights

Anders Celsius (born November 27, 1701, Uppsala, Sweden—died April 25, 1744, Uppsala) was an astronomer who invented the Celsius temperature scale (often called the centigrade scale).

Celsius was professor of astronomy at Uppsala University from 1730 to 1744, and in 1740 he built the Uppsala Observatory. In 1733 Celsius published a collection of 316 observations of the aurora borealis, or northern lights, made by himself and others from 1716 to 1732. He advocated the measurement of an arc of a meridian in Lapland and in 1736 took part in an expedition organized for that purpose, which verified Isaac Newton’s theory that the Earth is somewhat flattened at the poles. In 1742 he described his thermometer in a paper read before the Swedish Academy of Sciences. His other works include Dissertatio de Nova Methodo Distantiam Solis a Terra Determinandi (1730; “A Dissertation on a New Method of Determining the Distance of the Sun from the Earth”) and De Observationibus pro Figura Telluris Determinanda in Gallia Habitis, Disquisitio (1738; “Disquisition on Observations Made in France for Determining the Shape of the Earth”).

This article was most recently revised and updated by Encyclopaedia Britannica.
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temperature, measure of hotness or coldness expressed in terms of any of several arbitrary scales and indicating the direction in which heat energy will spontaneously flow—i.e., from a hotter body (one at a higher temperature) to a colder body (one at a lower temperature). Temperature is not the equivalent of the energy of a thermodynamic system; e.g., a burning match is at a much higher temperature than an iceberg, but the total heat energy contained in an iceberg is much greater than the energy contained in a match. Temperature, similar to pressure or density, is called an intensive property—one that is independent of the quantity of matter being considered—as distinguished from extensive properties, such as mass or volume.

Three temperature scales are in general use today. The Fahrenheit (°F) temperature scale is used in the United States and a few other English-speaking countries. The Celsius (°C) temperature scale is standard in virtually all countries that have adopted the metric system of measurement, and it is widely used in the sciences. The Kelvin (K) scale, an absolute temperature scale (obtained by shifting the Celsius scale by −273.15° so that absolute zero coincides with 0 K), is recognized as the international standard for scientific temperature measurement.

In certain fields of engineering, another absolute temperature scale, the Rankine scale (see William Rankine), is preferred over the Kelvin scale. Its unit of measure—the degree Rankine (°R)—equals the Fahrenheit degree, as the kelvin equals one Celsius degree.

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The Réaumur (°Re) temperature scale (or octogesimal division) was widely used in parts of Europe in the 18th and 19th centuries; it later was used primarily to measure the temperature of mixtures during brewing, of syrups in the production of certain food products, and of milk during cheese making.

This article was most recently revised and updated by Encyclopaedia Britannica.