No leap second for December 31, 2021
The International Earth Rotation and Reference Systems Service announced in July 2021 that there’d be no leap second added to the world’s official timekeeping in December 2021. The last leap second was December 31, 2016. Since they always add leap seconds on the last day of June or December, the next possible date for a leap second is June 30, 2022.
Timekeepers have added leap seconds 27 times since 1972. There were leap seconds added on June 30, 2015, and on June 30, 2012. They’re always added to the world’s clocks at 23 hours, 59 minutes and 59 seconds Coordinated Universal Time (UTC), on either June 30 or December 31.
The extra second is necessary for our official timekeeping mainly to keep our increasingly electronic world in sync.
Why do we need a leap second?
Isn’t the length of our day set by the rotation of the Earth? Like the ancients who insisted that all motion in the heavens must be perfect, uniform and unvarying, many of us today assume that the Earth’s rotation – its spin on its axis – is perfectly steady. We learned, correctly, that the sun, moon, stars and planets parade across our sky because the Earth turns. So it is easy to understand why we assume that the Earth’s rotation is precise and unwavering. Yet Earth’s rotation does not stay perfectly steady.
Instead, compared to modern timekeeping methods such as atomic clocks, the Earth is a notoriously poor timepiece. Overall, as many know, Earth’s spin is slowing down. The length of our day is increasing. The Wikipedia entry on this subject explains it well:
Earth’s rotation is slowing slightly with time; thus, a day was shorter in the past. This is due to the tidal effects the moon has on Earth’s rotation. Atomic clocks show that a modern day is longer by about 1.7 milliseconds than a century ago, slowly increasing the rate at which UTC is adjusted by leap seconds. Analysis of historical astronomical records shows a slowing trend; the length of a day increased about 2.3 milliseconds per century since the 8th century BCE.
Earth’s rotation is slowing, but it can also speed up
The fact is Earth’s rotation is subject to effects that are hard to predict. Other short-term and unpredictable changes result from a variety of events. These range from slight changes in the distribution of mass in the Earth’s molten outer core, to movement of large masses of ice near the poles, to density and angular momentum variations in the Earth’s atmosphere.
For example, you might recall the devastating Fukushima earthquake that struck in northeastern Japan in 2011. The quake was magnitude 9.0, the largest ever recorded in Japan. It was the world’s fourth-biggest earthquake since 1900. It unleashed a powerful tsunami that caused the death of some 16,000 people and caused a nuclear meltdown at Fukushima Daiichi Nuclear Power Plant. The quake also caused displacements of portions of the Earth’s crust that sped up Earth’s rotation, shortening the day by 1.6 millionth of a second.
The tides affect Earth’s rotation
If you have ever been to the beach, you will be familiar with the main reason our planet is slowing down. That reason is ocean tides. As our planet rotates, it plows past the great watery bulges (raised mostly by the gravitational interaction of the Earth and moon), which serves to slow it down much like a brake on a rotating wheel. This effect is small, actually very small. According to calculations based on the timing of ancient astronomical events (eclipses), the Earth’s rotation has slowed down by about 0.0015 to 0.002 seconds per day per century.
In other words, the days are becoming longer by about 0.002 seconds per day. But the rate at which this increase occurs also grows slowly over time. Currently that rate is also about 0.002 seconds, but per 100 years.
So the Earth is slowing down, very slowly. What happens, though, is that the daily 0.002-second difference between the original definition of a day (86,400 seconds) builds up.
After one day it is 0.002 seconds. After two days it is 0.004 seconds. By three days it is 0.006 seconds and so on. In about a year and a half, the difference mounts to about 1 second. It is this difference that has prompted the addition of a leap second.
Atomic clocks (which are accurate to about a billionth of a second per day) track all of this to an extremely high precision.
The inconstant Earth
Of course, the slowdown is not constant either. According to the U.S. Naval Observatory, from 1973 to 2008 the variation in Earth’s spin has ranged from plus 4 milliseconds to minus 1 millisecond. Over time, that could necessitate a negative leap second, signifying an increase in the Earth’s rotation speed.
But, since the concept of leap seconds began in 1973, this has never happened.
And, by the way, if this fine detail on timekeeping seems esoteric or unimportant to you, realize that it’s not to the telecommunications industry.
Not everyone thinks a leap second is a good idea
The International Telecommunications Union (ITU), a United Nations body that governs some global issues related to time, has been contemplating leap seconds for some time. They considered abolishing the practice, but in November 2015 – with delegates from more than 150 nations meeting in Geneva – the ITU announced it had decided not to dump the leap second, at least not right now. The ITU said:
The decision … calls for further studies regarding current and potential future reference time-scales, including their impact and applications. A report will be considered by the World Radiocommunication Conference in 2023.
So they’re still thinking about it.
Consider the ITU’s situation. Telecommunications relies on precise timing, and the addition of a leap second forces companies to turn off many systems for a second every year or two. To get all such systems in a global industry cycled on and off in sync can be a major headache. Consider also that the global positioning system (GPS) does not use the leap second system, which causes further confusion. Many in the industry feel that the periodic addition of a leap second to keep the two measurements in step is cumbersome and wasteful.
Although dropping the idea of a leap second would be a convenience for telecommunication and other industries, in the long (very long) run, it would cause clocks to get out of sync with the sun, eventually causing 12 p.m. (noon) to occur in the middle of the night, for example. At the current rate of change in Earth’s rotation rate, it would take about 5,000 years to amass just a one-hour difference between the Earth’s actual rotation rate and the atomic clock.
Measuring the spin difference
How, you may ask, do we even measure such small changes in the Earth’s rotation? Historically, astronomers (such as those at Britain’s famed Royal Greenwich Observatory near London) have used a telescope to watch a star pass through their eyepiece, crossing an imaginary line called the meridian. Then they time how long it takes for the Earth to bring that star back around to cross the meridian again. This is highly accurate for everyday purposes. For science, it’s not good enough. The wavelengths and the murkiness of the atmosphere limit its accuracy.
A much more accurate method is to use two or more radio telescopes separated by thousands of miles in a technique called very long baseline interferometry. By carefully combining the data from each of the telescopes, astronomers effectively have a telescope thousands of miles in size, which provides much greater resolution (detecting fine detail) and measurement of position. This allows them to determine the planet’s rotation rate to an accuracy of less than a thousandth of a second. They do not observe stars, however, but very distant objects called quasars. The NASA video below will tell you more …
Bottom line: World timekeepers have decreed there will be no leap second on December 31, 2021. Overall the spin of Earth is slowing down, but in 2020 it sped up. They will consider a proposal to dump the leap second in 2023. Stay tuned!