The Creation of Standard Time

Since the late 19th century, the Prime Meridian at Greenwich has served as the reference line for Greenwich Mean Time. Before this, almost every town in the world kept its own local time. There were no national or international conventions which set how time should be measured, or when the day would begin and end, or what length an hour might be. However, with the vast expansion of the railway and communications networks during the 1850s and 1860s, the worldwide need for an international time standard became imperative.

What is UTC and all that stuff?

The times of astronomical and weather phenomena and events that are observed internationally (by treaty, for example) are often given in "Universal Time" (abbreviated (UTC) or "Greenwich Mean Time" (abbreviated GMT). The two terms are often used synonymously to refer, loosely, to time kept on the Greenwich meridian (longitude zero), five hours ahead of Eastern Standard Time.
However, when a precision of one second or better is needed, it is important to know that UTC and GMT have slightly different meanings for astronomical phenomena and civil affairs, as explained below. In either case, times given in UTC or GMT are almost always given in terms of a 24 hour clock. Thus, 14:42 (often written simply 1442) is 2:42 p.m., and 21:17 (2117) is 9:17 p.m. Sometimes a Z is appended to a time to indicate GMT, as in 0935Z.

However, in normal civil usage, UTC or GMT refers to a time scale called "Universal Time, Coordinated" (abbreviated UTC), which is the basis for the worldwide system of civil time.
The UTC time scale is kept by a large number of highly precise atomic clocks at facilities around the world, including the U.S. Naval Observatory, and there is international coordination in maintaining UTC to better than a nanosecond (billionth of a second) per day. The length of a UTC second is defined in terms of a count of radiation cycles of a certain atomic transition of the element cesium, and is not directly related to any astronomical phenomena.

What is a Meridian?

A meridian is a north south line selected as the zero reference line for astronomical observations. By comparing thousands of observations taken from the same meridian it is possible to build up an accurate map of the sky.

Hemispheres?

The line in Greenwich represents the Prime Meridian of the World - Longitude 0º. Every place on Earth is measured in terms of its distance east or west from this line. The line itself divides the eastern and western hemispheres of the Earth - just as the Equator divides the northern and southern hemispheres. East longitudes are positive, west longitudes are negative.
 
To obtain: 
Atlantic Daylight Time Subtract 3 hours from UTC
Atlantic Standard Time  Subtract 4 hours from UTC
Eastern Daylight Time  Subtract 4 hours from UTC
Eastern Standard Time Subtract 5 hours from UTC
Central Daylight Time Subtract 5 hours from UTC
Central Standard Time Subtract 6 hours from UTC
Mountain Daylight Time Subtract 6 hours from UTC
Mountain Standard Time  Subtract 7 hours from UTC
Pacific Daylight Time Subtract 7 hours from UTC
Pacific Standard Time  Subtract 8 hours from UTC
Alaska Daylight Time Subtract 8 hours from UTC
Alaska Standard Time  Subtract 9 hours from UTC
Hawaii Aleutian Daylight Time  Subtract 9 hours from UTC
Hawaii Aleutian Standard Time Subtract 10 hours from UTC
Samoa Standard Time Subtract 11 hours from UTC

Thus, 11:00 UTC is the same as 5:00 CST. When converting zone time to or from UTC, dates must be properly taken into account. For example, 10 March at 02:00 UTC is the same as 9 March at 21:00 EST. The table can also be used to determine the difference between the time observed in any two zones. For example, the table shows that Eastern Standard Time is three hours "ahead" of Pacific Standard Time.

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