Time Synchronisation

We may think of their being only one time and therefore one timescale. Sure, we’re all aware of time zones where the clock has to be pushed back an hour but we all obey the same time surely?

Well actually we don’t. There are numerous different timescales all developed for different reasons are too numerous to mention them all but it wasn’t until the nineteenth century that the idea of a single timescale, used y everybody came into effect.

It was the advent of the railway that provoked the first national timescale in the UK (Railway time) before then people would use noon as a basis for time and set their clocks to it. It rarely mattered if your watch was five minutes faster than your neighbours but the invention of the trains and the railway timetable soon changed all that.

The railway timetable was only useful if people all used the same time scale. A train leaving at 10.am would be missed if a watch was five minutes slow so synchronisation of time became a new obsession.

Following railway time a more global timescale was developed GMT (Greenwich Meantime) which was based on the Sun’s position at noon which fell over the Greenwich Meridian line (0 degrees longitude). It was decided during a world conference in 1884 that a single world meridian should  replace the numerous one’s already in existence. London was perhaps the most successful city in the world so it was decided the best place for it.

GMT allowed the entire world to synchronise to the same time and while nations altered their clocks to adjust for time-zones their time was always based on GMT.

GMT proved a successful development and remained the world’s global timescale until the 1970’s. By then that atomic clock had been developed and it was discovered in the use of these devices that Earth’s rotation wasn’t a reliable measure to base our time on as it actually alters day by day (albeit by fractions of a second).

Because of this a new timescale was developed called UTC (Coordinated Universal Time). UTC is based on GMT but allows for the slowing of the Earth’s rotation by adding additional ‘Leap Seconds’ to ensure that Noon remains on the Greenwich Meridian.

UTC is now used all over the World and is essential for applications such as air traffic control, satellite navigation and the Internet. In fact computer networks across the globe are synchronised to UTC using NTP time servers (Network Time Protocol). UTC is governed by a constellation of atomic clocks controlled by national physics laboratories such as NIST (National Institute of Standards and Time) and the UK’s NPL.

A global economy has many benefits allowing trade and commerce to be conducted relatively pain free from the other sides of the planet. But conducting business with other countries can have its problems most notably time differences.

We are used to the fact that when we go to bed in Europe, those in Australasia are jest getting up and for many businesses, knowing the time in the country that you trade in is essential. However many global transactions are now conducted online and quite often completely automated.

For this reason computers need to know the exact time too, particularly if they are selling products and services that have a limited quantity and any miscalculation in the time can cause untold errors. For instance, if people across the globe wish to buy an airline ticket from an American broker then the computer needs to know who ordered the seat first otherwise there could be a risk of double-booking.

For this reason a global timescale has been developed allowing the whole world to synchronise to one timescale. This global timescale is commonly known as UTC (Coordinated Universal Time) and is based onthe old timescale GMT (Greenwich Meantime) although it accounts for the slowing of the Earth due to tidal and lunar forces.

UTC is kept accurate by atomic clocks that boast an accuracy of a second every 100 million years, however, atomic clocks are highly expensive to own, operate and run and are therefore impractical for a business that just wants to keep accurate UTC.

For this reason the dedicated NTP time server has been developed that can receive a transmitted time signal from an atomic clock and synchronise an entire computer network to it.

The NTP time server can receive a time signal directly from a physic laboratory using a long wave receiver or more conveniently using the GPS signals that are transmitted by satellites 30,000 km above the Earth.

By using a NTP time server a business network can be kept to within a few milliseconds of UTC (thousandth of seconds) ensuring that they can trade and do business with complete and accurate synchronisation.

We may think of their being only one time and therefore one timescale. Sure, we’re all aware of time zones where the clock has to be pushed back an hour but we all obey the same time surely?

Well actually we don’t. There are numerous different timescales all developed for different reasons are too numerous to mention them all but it wasn’t until the nineteenth century that the idea of a single timescale, used by everybody came into effect.

It was the advent of the railway that provoked the first national timescale in the UK (Railway time) before then people would use noon as a basis for time and set their clocks to it. It rarely mattered if your watch was five minutes faster than your neighbours but the invention of the trains and the railway timetable soon changed all that.

The railway timetable was only useful if people all used the same time scale. A train leaving at 10.am would be missed if a watch was five minutes slow so synchronisation of time became a new obsession.

Following railway time a more global timescale was developed GMT (Greenwich Meantime) which was based on the Sun’s position at noon which fell over the Greenwich Meridian line (0 degrees longitude). It was decided during a world conference in 1884 that a single world meridian should  replace the numerous one’s already in existence. London was perhaps the most successful city in the world so it was decided the best place for it.

GMT allowed the entire world to synchronise to the same time and while nations altered their clocks to adjust for time-zones their time was always based on GMT.

GMT proved a successful development and remained the world’s global timescale until the 1970’s. By then that atomic clock had been developed and it was discovered in the use of these devices that Earth’s rotation wasn’t a reliable measure to base our time on as it actually alters day by day (albeit by fractions of a second).

Because of this a new timescale was developed called UTC (Coordinated Universal Time). UTC is based on GMT but allows for the slowing of the Earth’s rotation by adding additional ‘Leap Seconds’ to ensure that Noon remains on the Greenwich Meridian.

UTC is now used all over the World and is essential for applications such as air traffic control, satellite navigation and the Internet. In fact computer networks across the globe are synchronised to UTC using NTP time servers (Network Time Protocol). UTC is governed by a constellation of atomic clocks controlled by national physics laboratories such as NIST (National Institute of Standards and Time) and the UK’s NPL.

Apart from the usual celebrations and revelry the end of December brought with the addition of another Leap Second to UTC time (Coordinated Universal Time).

UTC is the global timescale used by computer networks across the world ensuring that everybody is keeping the same time. Leap Seconds are added to UTC by the International Earth Rotation Service (IERS) in response to the slowing of the Earth’s rotation due to tidal forces and other anomalies. Failure to insert a leap second would mean that UTC would drift away from GMT (Greenwich Meantime) – often referred to as UT1. GMT is based on the position of the celestial bodies so at midday the sun is at its highest above the Greenwich Meridian.

If UTC and GMT were to drift apart it would make life difficult for people like astronomers and farmers and eventually night and day would drift (albeit in a thousand years or so).

Normally leap seconds are added to the very last minute of December 31 but occasionally if more than one is required in a year then is added in the summer.

Leap seconds, however, are controversial and can also cause problems if equipment isn’t designed with leap seconds in mind. For instance, the most recent leap second was added on 31 December and it caused database giant Oracle’s Cluster Ready Service to fail. It resulted in the system automatically rebooting itself on New Year.

Leap Seconds can also cause problems if networks are synchronised using Internet time sources or devices that require manual intervention.  Fortunately most dedicated NTP servers are designed with Leap Seconds in mind. These devices require no intervention and will automatically adjust the entire network to the correct time when there is a Leap Second.

A dedicated NTP server is not only self-adjusting requiring no manual intervention  but also they are highly accurate being stratum 1 servers (most Internet time sources are stratum 2 devices in other words devices that receive time signals from stratum 1 devices then reissue it) but they are also highly secure being external devices not required to be behind the firewall.

The NTP server or network time server as it is often called is the culmination of centuries of horology and chronology. The history of keeping track of time has not been as smooth as you may think.

What month was the Russian October revolution? I’m sure you have guessed that it is a trick question, in fact if you trace the days back to the October revolution that changed the shape of Russia in 1917 you will find it didn’t start until November!

One of the first decisions the Bolsheviks, who had won the revolution, chose to make was to join the rest of eh world by taking up the Gregorian calendar. Russia was last to do adopt the calendar, which is still in use throughout the world today.

This new calendar was more sophisticated that the Julian calendar which most of Europe had been using since the Roman Empire. Unfortunately the Julian calendar did not allow for enough leap years and by the turn of the century this had meant that the seasons had drifted, so-much-so, that when Russia finally adopted the calendar on after Wednesday, 31 January 1918 the following day became Thursday, 14 February 1918.

So whilst the October revolution occurred in October in the old system, to the new Gregorian calendar it meant it had taken place in November.

Whilst the rest of Europe adopted this more accurate calendar earlier than the Russians they still also had to correct the seasonal drift, so in 1752 when Britain changed systems they lost eleven days which according to the populist painter of the time, Hogarth, caused rioters to demand the return of their lost eleven days.

This problem of inaccuracy in keeping track of time was thought to be solved in the 1950’s when the first atomic clocks were developed. These devices were so accurate that they could keep time for a million years without losing a second.

However, it was soon discovered that these new chronometers were in fact too accurate – compared with the Earth’s rotation anyway. The problem was that while atomic clocks could measure the length of a day to the nearest millisecond, a day is never the same length.

The reason being is that the Moon’s gravity affects the Earth’s rotation causing a wobble. This wobble has the effect of slowing down and speeding up the Earth’s spin. If nothing was done to compensate for this then eventually the time told by atomic clocks (International Atomic Time- TAI) and the time based on the Earth’s rotation used by farmers, astronomers and you and I (Greenwich Meantime- GMT) would drift that eventually noon would become midnight (albeit in many millennia).

The solution has been to devise a timescale that is based on atomic time but also accounts for this wobble of the Earth’s rotation. The solution was called UTC (Coordinated Universal Time) and accounts for the Earth’s variable rotation by having ‘leap seconds’ occasionally added. There have been over thirty leap seconds added to UTC since its inception in the 1970’s.

UTC is now a global timescale used throughout the world by computer networks to synchronise too. Most computer networks use a NTP server to receive and distribute UTC time.

The NTP timescale is based on UTC (Coordinated Universal Time) which is a global civil timescale that is based on International Atomic Time (TAI) but accounts for the slowing of the Earth’s spin by intermittingly adding ‘leap seconds.’

This is done to ensure that UTC is kept in coincidence with GMT (Greenwich Meantime, often referred to as UT1). Failing to account for the Earth’s slowing in its rotation (and occasional speeding up) would mean that UTC would fall out of synchronisation with GMT and noon, when the sun is traditionally the highest in the sky would drift. In fact if leap seconds were not added eventually noon would fall at midnight and vice versa (albeit in several millennia).

Not everybody is happy with leap seconds, there are those that feel that adding of seconds to keep the Earth’s rotation and UTC inline is nothing but a fudge. However, failing to do so would make such things as astronomical observations impossible as astronomers need to know the exact positioning of the stellar bodies and farmers are pretty reliant on the Earth’s rotation too.

The NTP clock represents time in a totally different way to the way humans perceive time. Instead of formatting time into minutes, hours, days, months and years, NTP uses a continuous number that represents the number of seconds that have past since 0h 1 January 1900. This is known as the prime epoch.

The seconds counted from the prime epoch continue to rise but wraps around every 136 years. The first wrap-around will take place in 2036, 136 years since the prime epoch. To deal with this NTP will utilise an era integer, so when the seconds reset to zero, the integer 1 will represent the first era and negative integers represent the eras before the prime epoch.

Time servers that receive their time from the GPS system are not in fact receiving UTC, primarily because the GPS network was in development before the first leap second but they are based on TAI.  However, GPS time is converted to UTC by the GPS time server.

The radio transmission broadcast from national physics laboratories such as MSF, DCF or WWVB are all based on UTC and so the time servers do not need to do any conversion.

How do you set the time on your watch? From the speaking clock, the chimes of Big Ben perhaps but have you wondered where they get the time from?

There is no master clock that the world relies on but there is a global timescale called UTC (Coordinated Universal Time). UTC was developed after the development of atomic clocks. It is based on a combination of International Atomic Time (TAI – the time told by these clocks) and Greenwich Meantime (GMT).

While TAI is incredibly accurate it is actually too accurate as the Earths rotation slows due to the effect of the moon’s gravity. It compensates for this by adding Leap Seconds to keep in similar to GMT, otherwise night would creep into day.

UTC is governed by a constellation of atomic clocks all over the world to ensure even more accuracy (and to prevent any political squabbles).

A NTP Time Server is a device that can receive UTC time through either a radio transmission (in certain countries) or the GPS network. NTP (Network Time Protocol) is designed to synchronise all devices on a network to the time received by the NTP time server.

A NTP time server allows networks all over the world to communciate safely synchronised to the exact same time.

UTC and NTP time servers allow the whole world to communicate within the same timescale. Without them, many of the applications and processes we do online would be impossible such as Internet trading, the stock exchange, buying airline tickets and even sending and receiving email.

Keeping track of time is something most people take for granted, yet the science of timekeeping has a long and fascinating history.

Keeping track of time was always based on the relationship between the Earth, Moon and Sun. The first timekeeping devices are thought to be monuments like Stone Henge in the UK that would recognise the winter or summer solstice allowing early man to calculate when to plant crops.

Dividing the day up into hours and being able to keep track of them has proved more difficult to civilisations.

The first timing devices were sundials, obelisks and water clocks but it wasn’t until the development of mechanical clocks in the middle-ages that time-telling started to become more accurate.

Mechanical clocks continued to develop until the turn of the twentieth century when they were bettered in accuracy by electronic oscillators that would use the resonance of a crystal (often quartz) to keep a stable time.

While electronic clocks provided accuracy to within a second a day, the atomic clock that uses the resonance of an atom (in most cases caesium -133) and was developed in the 1950’s demonstrated millisecond accuracy – not losing a second in several thousands of years.

Now atomic clocks are approaching nano-second accuracy (one second every billion years) with new developments like strontium. The atomic clock has also made horologists realise that basing a time system on the movement of the Earth and celestial bodies is unreliable as the Earth slows and speeds up.

UTC (coordinated universal time) was developed to combat this by adding leap seconds to keep atomic time in line with GMT (Greenwich Meantime). Now computer networks all over the world can synchronise to UTC and atomic clocks by using a time server.

A time server will receive a time from an atomic clock source and synchronise an entire network to this time. Without time servers, atomic clocks and UTC, technologies such as satellite communication, the Internet and global trading would be near impossible.

The atomic clock was developed in the 1950’s and represented a huge step forward in chronology. Before the atomic clock, electronic oscillators, as used in most digital clocks and watches, were providing the best accuracy although these would drift several seconds a month.

The atomic clock used the resonance of the atom caesium -133 which had an exact oscillation of 9,192,631,770 times a second. Because of this exact oscillation atomic clocks soon offered nearnano-second accuracy in that it would take several million years before they would drift by a second.

Atomic clocks were deemed so accurate that the International System of Units (SI) defined the second as this number of oscillations of the caesium atom.

As time-telling became so accurate it was soon discovered that the rotation of the Earth was not as precise as the clocks and that to keep atomic time relevant to Greenwich Meantime (GMT) and to stop night from slowly drifting into day a new timescale was developed calledUTC (Coordinated Universal Time) which accounted for the slowing of the Earth’s spin by adding ‘Leap Seconds’.

UTC is now globally used and allows the entire world to synchronise to the same timescale. This is particularly relevant for computer networks that often have to communicate with other networks across the globe.

UTC can be received by using a time server that can either synchronise to a timing reference across the Internet or for better accuracy an d security a time server can receiveUTC time from the GPS network via a GPS antenna or by receiving national timing broadcasts, transmitted form several countries.

By using a time server that receives UTC time a computer network can be accurate to within a few milliseconds of UTC allowing cross-global communication.

Most people have heard of atomic clocks, their accuracy and precision are well known. An ato0mic clock has the potential to keep time for several hundred million years and not lose a second in drift. Drift is the process where clocks lose or gain time because of the inaccuracies in the mechanisms that make them work.

Mechanical clocks, for instance, have been around for hundreds of years but even the most expensive and well engineered will drift at least a second a day. Whilst electronic clocks are more accurate they also will drift by about a second a week.

Atomic clocks have no comparison when it comes to time keeping. Because an atomic clock is based on the oscillation of an atom (in most cases the caesium 133 atom) which has an exact and finite resonance (caesium is 9,192,631,770 every second) this makes them accurate to within a billionth of a second (a nanosecond).

While this type of accuracy is unparalleled it has made possible technologies and innovations that have changed the world. Satellite communication is only possible thanks to the time keeping of atomic clocks, so is satellite navigation. As the speed of light (and therefore radio waves) travel at over 300,000km a second an inaccuracy of a second could see a navigation system be hundreds of thousands of miles out.

Precise accuracy is also essential in many modern computer applications. Global communication, particularly financial transactions have to be done precisely. In Wall Street or the London stock exchange a second can see the value of stock rise or fall by millions. Online reservation also requires the accuracy and perfect synchronisation only atomic clocks can provide otherwise tickets could be sold more than once and cash machines could end up paying out your wages twice if you found a cash machine with a slow clock.

Whilst this may sound desirable to the more dishonest of us, it doesn’t take much imagination to understand what problems a lack of accuracy and synchronisation could cause. For this reason an International timescale based on the time told by atomic clocks has been developed.

UTC (Coordinated Universal Time) is the same everywhere and can account for the slowing of the Earth’s rotation by adding leap seconds to keep UTC inline with GMT (Greenwich Meantime). All computer networks that participate in global communication need to be synchronised to UTC. Because UTC is based on the time told by atomic clocks it is the most precise timescale possible. For a computer network to receive and keep synchronised to UTC  it first needs access to an atomic clock. These are expensive and large pieces of equipment and are generally only to be found in large scale physics laboratories.

Fortunately the time told by these clocks can still be received by a network time server wither by utilising time and frequency long wave broadcasts transmitted by national physics laboratories or from the GPS (Global Positioning system). NTP (network time protocol) can then distribute this UTC time to the network and use the time signal to keep all devices on the network perfectly synchronised to UTC.