We don't think about time zones much when we are at home in the US. We all know that California is three time zones away from the East Coast, but for the most part we don't give them much thought.
President Chester A. Arthur |
The imposition is all that much greater when one flies home or returns to Central Asia. The human body just wasn't designed to absorb a 10-11 hour time difference in the blink of an eye unless, of course, it takes a week or ten days to blink that eye.
It wasn't always this way, you know. Two hundred years ago there were no time zones. Each major city maintained its own time based on the daily passage of the Sun across the meridian, the line that connects due North with due South that passes through the zenith. Life was easy. When the Sun was on the meridian, it was noon. It's what we would call today local apparent time. The time it took to travel from one city to another in Europe or the American colonies was so great that the local definition of time in any one city was not an issue.
Things began to change in the early nineteenth century. By then local mean time had begun to replace local apparent time. Instead of the actual, physical Sun, the mean Sun's passage through the meridian is what determined the noon hour. It had long been noted that the physical Sun sometimes took more than 24 hours between meridian crossings, sometimes less, with the deviation reaching as much as 16 minutes.
“The reason?”
“Why, it's elementary, dear Newton!”
This discrepancy is caused first of all by the 23.44-deg obliquity of the ecliptic, the angle between the Earth's equator and the plane of the Earth's orbital motion around the Sun. Secondly, the Earth's orbit is not exactly circular but is, rather, an ellipse, which means that the Earth's orbital motion around the Sun is faster at the time of perihelion -- closest approach to the Sun -- than it is six months later at aphelion.
The U.S. experience in the mid-ninteenth century was quickly being replicated in much of the industrialized world. It was compounded by the circumstance that different countries were using different prime meridians relative to which to measure longtitude and time. France used the Paris meridian. Russia used the Pulkovo meridian. Great Britain measured longtitude from Greenwich. The US at times used the meridian of the U.S. Naval Observatory. Several meetings and conferences were held beginning in the mid-nineteenth century to try to resolve the joint problem of standardized time and longitude. In 1870, U.S. educator Charles F. Dowd proposed a system of U.S. time zones. He was followed a few years later by Canadian railroad engineer Sanford Fleming who proposed that there be a worldwide system of time zones.
Delegates to the International Meridian Conference |
The Greenwich Meridian |
Is it all over? Has time been resolved for all civil purposes? Well, not really. For the answer to that and more, look for a possible future entry on atomic time, Coordinated Universal Time, and leap seconds. The story is just beginning.
(Dramatic foreshadowing: Greenwich Mean Time has not existed as an intenational time standard since Richard Nixon was President of the US.)
Of course, Albert Einstein would tell you that time passed slower in the airplane than on the ground!
ReplyDeleteAnd both he and you would be right!
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