Time clock standards

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The western time standards dividing the year into 12 months, the day into 24 hours or 12 hours AM and 12 hours PM, the hour into 60 minutes and the hour into 60 seconds derived from the Mesopotamia[1] using the sexagesimal[2] or base 60 numeral system.

Note:
The base 60 systems is a highly composite number as 1, 2, 3, 4, 5, 6, 10, 12, 15, 20, 30 and 60 are factors.

The length of a day

Defined in ISO 8601 the day consists of 24 hours consisting of 60 minutes of 60 seconds. giving a total of <math>24 * 60 * 60 = 86400 seconds</math> a day. With the Earth rotation slowing down there are two possible ways to make the clock time match the rotation of the Earth.

  1. Decreasing the length of the second to match 86400 second/day
  2. Introducing a leap second[3] when needed.

DST or summer time

World map. Europe, Russia, most of North America, parts of southern South America and southern Australia, and a few other places use DST. Most of equatorial Africa and a few other places near the equator have never used DST. The rest of the land mass is marked as formerly using DST.
Although not used by the majority of the world's countries, daylight saving time is common in the Western world.
  DST is used.
  DST is no longer used.
  DST has never been used.

Daylight saving time (DST)[4]—also summer time in British English— is the practice of advancing clocks during the lighter months so that evenings have more daylight and mornings have less. Typically clocks are adjusted forward one hour near the start of spring and are adjusted backward in autumn.

References

  1. ↑ Mesopotamia Mathematics
  2. ↑ Sexagesimal or base 60 numeral system
  3. ↑ Leap_second
  4. ↑ Daylight saving time
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