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Decimal Time - HistoryEgypt
The ancient Egyptians divided each daily period of sunlight into ten hours,
marked by sundials.
They had an additional hour of twilight before sunrise and one after sunset,
for a total of twelve hours of light. The night was also divided into twelve
hours, marked by certain stars, for a total of 24 hours. The use of sundials
to tell time became common in many places, which resulted in hours being
variable in length during the year, becoming longer in the summer and shorter
in the winter. The invention of mechanical clocks in the Middle Ages, which
ran at fairly constant rates, finally led to hours of equal length.
At first the hours were divided roughly into halves and quarters, but the
addition of another clock hand allowed the hour to be divided more finely.
The first hand revolved around the clock dial twice per day, with the dial
divided into twelve hours.
The second hand revolved once per hour, dividing the hour into twelve
parts. Each twelfth-hour was then divided by five by adding four marks between
the hour marks, thus dividing the hour into sixty parts. This mirrored the
Babylonian sexigesimal system, which was already used to measure angles.
The Babylonians divided the circle into six parts, each equal to the angle of an equilateral
triangle, which was divided into 60 degrees. Each degree was divided into
60 smaller parts, and so on. The first division of the degree was called a
minute, from the Latin pars minuta, meaning "small part". One sixtieth
of a minute was called a second from pars minuta secunda, because it
was the 2nd level of division.
(Even greater levels of angular division have sometimes been used, called
"thirds", etc.) Divisions of the clock hour were based on the ancient
Babylonian divisions of the degree, first by adding a minutes hand, and later
also a seconds hand.
Originally clocks displayed local solar time, and were set to twelve o'clock
when the sun reached its highest point of the day. However, the length of
the day varied slightly during the year, so that this might happen as much
as a quarter-hour before or after the mean solar noon. In addition, clocks
varied as one travelled east or west, according to the curve of the earth.
With the invention of instant communication via telegraph and rapid travel
via railroad, the time of an entire country was usually synchronized with
that of its capital city. For instance, in the United Kindom the time was
kept at the Royal Observatory at Greenwich, near London. In 1884 the
International Meridian Conference was held in Washington,
DC, which established hourly
offsets from Greenwich mean time as Standard Time, so that local Standard
Time is usually within a half-hour of mean solar time, establshing synchronized
zones hundreds of miles wide.
This was immediately adopted in the United States, and eventually in the rest
of the world, although some countries use intermediate offsets.
This was modified in some places during the twentieth century by shifting the time during
part of the year by one hour, so that the sun rises and sets later according
to the clock when there are more hours of daylight; this is called Daylight
Saving Time or Summer Time.
The ancient Chinese used clepsydras or water clocks to divide the day into 100 units called ke, each equal to 14 minutes and 24 seconds, which existed alongside a system which divided the day into 12 double-hours, named for the "earthly branches". After European time was introduced, a quarter-hour came to be called a ke. During the French Revolution, the National Convention passed a law on October 5, 1793, establishing the Republican Calendar with 10-day décades instead of 7-day weeks, which also included an article defining decimal time. This article was modified slightly by the law of November 24, 1793, (which also named the months of the new calendar, the first month being named Vendémiaire) with the addition of the underlined words: Which translates into English as: Thus, French decimal time was originally defined simply as a decimal fraction of the day, which was later modified with the definitions of decimal time units (decimal hours, minutes and seconds) to resemble traditional timekeeping. Each multiple of ten decimal minutes was sometimes called a décime, because it was one-tenth of a decimal hour, and which was conveniently close to an old-style quarter-hour. On August 22, 1794, a contest was held for designs to convert clocks and watches to the new style, to be judged by Ferdinand Berthoud, Antide Janvier, and Jean Antoine Lépine. Clocks and watches were built with decimal dials, most displaying both 10 and 24 hours. The hours were numbered 1-10, with 10 for midnight and 5 for noon. The modern convention of separating units with colons (:) was not in common use then, and even today it is still common in France to state the time in heures (hours) and minutes (if any) and to abbreviate it by separating the hours and minutes with the letter h; e.g. 10 o'clock (10:00) is written as "10 heures" or "10h00". During the Revolution, decimal times were indicated by adding décimales, e.g. one written account from the eighth year of the Republic gives the decimal time as deux heures 10 minutes décimales (two hours 10 minutes decimal) along with the old style equivalent: cinq heures du matin (five hours of the morning). However, about six months after decimal time became mandatory for public acts, the metric system law of 18 Germinal, an III, (April 7, 1795) declared: Which means: However, although it was no longer mandatory, official records, such as births, deaths and marriages, continued to be recorded with decimal times in some parts of France for a number of years. The 10-day décades were replaced with 7-day weeks in April of 1802, and the Gregorian calendar finally reinstated on January 1, 1806. The French made another attempt at the decimalization of time in 1897, when the Commission de décimalisation du temps was created by the Bureau of Longitude, with the mathematician Henri Poincaré as secretary. The proposed unit of time was the standard hour of 1/24 day, divided into 100 minutes, and each minute into 100 seconds. However, this effort failed to gain any acceptance. By the nineteenth century astronomers were using fractional days. In 1849, the British astronomer, John Herschel, published Outlines of Astronomy, describing fractional days and also introducing a system of decimal dates, by counting days of the Julian Period. Astronomers began adding fractional days to Julian Days, which together are called Julian Dates. Astronomers then started and ended the day at noon, so Julian Dates also started and ended at noon, as observed in Greenwich, England, where the Prime Meridian was agreed to cross by an international conference in Washington, DC, in 1884. Since 1925, astronomers have started and ended the day at midnight, Greenwich Mean Time, so astronomers introduced Modified Julian Dates and other variations which are synchronized with the Universal Day. Also at the International Meridian Conference of 1884, the following resolution was passed, at the proposal of the French delegation: This resolution has yet to be carried out. |
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