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Published on June 30th, 2012 | by James Ayre

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‘Leap Second’ Saturday Night Will Make A 61-Second Minute (VIDEO)

 
20120629-230009.jpgOn Saturday night, ‘time’ will stand still for one second, as a ‘leap second’ is added to the regular 60-second minute.

The atomic clocks we use to measure time are extremely accurate, but the Earth’s rotation isn’t, so periodically, we readjust the International Atomic Time to better match ‘noon’ with the time of the day when the sun is at its highest in the sky. This discrepancy occurs because the rotation of the Earth is slowing very slightly every year, from tidal forces caused by the moon.

So, on Saturday (June 30, 2012), there will be an extra second, or ‘leap’ second, added at midnight “to account for the fact that it is taking Earth longer and longer to complete one full turn—a day—or, technically, a solar day.”

“The solar day is gradually getting longer because Earth’s rotation is slowing down ever so slightly,” says Daniel MacMillan of NASA’s Goddard Space Flight Center in Greenbelt, Md.

The exact amount of time it takes the Earth to rotate is known because researchers have been measuring it for decades, by using an extremely precise technique called the Very Long Baseline Interferometry (VLBI). “VLBI measurements are made daily by an international network of stations that team up to conduct observations at the same time and correlate the results. NASA Goddard provides essential coordination of these measurements, as well as processing and archiving the data collected. And NASA is helping to lead the development of the next generation of VLBI system through the agency’s Space Geodesy Project, led by Goddard.”

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Because of VLBI, researchers have learned that the Earth rotation is not a very accurate timekeeper. The Earth’s rotation is slowing down “because of tidal forces between Earth and the moon. Roughly every 100 years, the day gets about 1.4 milliseconds, or 1.4 thousandths of a second, longer. Granted, that’s about 100 or 200 times faster than the blink of an eye. But if you add up that small discrepancy every day for years and years, it can make a very big difference indeed.”

“At the time of the dinosaurs, Earth completed one rotation in about 23 hours,” says MacMillan, who is a member of the VLBI team at NASA Goddard. “In the year 1820, a rotation took exactly 24 hours, or 86,400 standard seconds. Since 1820, the mean solar day has increased by about 2.5 milliseconds.”

In the 1950s, researchers had realized that a more exact timekeeping method was needed for some scientific measurements and technologies. “So, in 1967, they officially changed the definition of a second. No longer was it based on the length of a day but on an extremely predictable measurement made of electromagnetic transitions in atoms of cesium. These ‘atomic clocks’ based on cesium are accurate to one second in 1,400,000 years. Most people around the world rely on the time standard based on the cesium atom: Coordinated Universal Time (UTC).”

Universal Time 1 (UT1), is another widely used time standard, based on “the rotation of Earth on its axis with respect to the sun. UT1 is officially computed from VLBI measurements, which rely on astronomical reference points and have a typical precision of 5 microseconds, or 5 millionths of a second, or better.”

“These reference points are very distant astronomical objects called quasars, which are essentially motionless when viewed from Earth because they are located several billion light years away,” says Goddard’s Stephen Merkowitz, the Space Geodesy Project manager.

“For VLBI observations, several stations around the world observe a selected quasar at the same time, with each station recording the arrival of the signal from the quasar; this is done for a series of quasars during a typical 24-hour session. These measurements are made with such exquisite accuracy that it’s actually possible to determine that the signal does not arrive at every station at exactly the same time. From the miniscule differences in arrival times, scientists can figure out the positions of the stations and Earth’s orientation in space, as well as calculating Earth’s rotation speed relative to the quasar positions.”

One of the original reasons leap seconds entered into used was to provide a UTC time signal that could be used for navigation at sea. This necessity of course become unimportant after the development of the GPS (Global Positioning System) and other forms of satellite navigation. So, currently, a leap second is inserted in UTC to keep it within 0.9 seconds of UT1.

“Normally, the clock would move from 23:59:59 to 00:00:00 the next day. Instead, at 23:59:59 on June 30, UTC will move to 23:59:60, and then to 00:00:00 on July 1. In practice, this means that clocks in many systems will be turned off for one second.”

“Proposals have been made to abolish the leap second and let the two time standards drift apart. This is because of the cost of planning for leap seconds and the potential impact of adjusting or turning important systems on and off in synch. No decision will made about that, however, until 2015 at the earliest by the International Telecommunication Union, a specialized agency of the United Nations that addresses issues in information and communication technologies. If the two standards are allowed to go further and further out of synch, they will differ by about 25 minutes in 500 years.”

For now though, leap seconds will continue to be added to the official UTC timekeeping. This will be the 35th leap second added altogether, and the first one since 2008.

Source: NASA
Image Credits: NASA, U.S. Navy/PMRF




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About the Author

James Ayre's background is predominantly in geopolitics and history, but he has an obsessive interest in pretty much everything. After an early life spent in the Imperial Free City of Dortmund, James followed the river Ruhr to Cofbuokheim, where he attended the University of Astnide. And where he also briefly considered entering the coal mining business. He currently writes for a living, on a broad variety of subjects, ranging from science, to politics, to military history, to renewable energy. You can follow his work on Google+.



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