Atomic clock
Adapted from Wikipedia · Adventurer experience
An atomic clock is a special kind of clock that measures time by watching the vibrations of atoms. Atoms have steady patterns, and these help scientists keep track of time very precisely. This exact way of measuring time helps define the second, the basic unit of time that we all use.
Because atomic clocks are so accurate, they are important for many things. They help keep our world time system, called UTC, matching the Earth's movement. This means that when you look at the time on your phone or watch, it stays correct over long periods.
Atomic clocks are also used in systems that help us find our way, like the GPS that cars and phones use. Even a tiny mistake in time, like one-billionth of a second, can make a big difference in knowing exactly where we are on Earth.
Today, many atomic clocks use a special type of atom called caesium, cooled to very cold temperatures to work at their best. For example, in the United States, there is a famous clock called NIST-F2 that is extremely precise, helping to set the standard for time around the world.
Recent advances
In July 2025, scientists in the United States made a big step in timekeeping. They built a very precise clock using a single trapped aluminium ion. This new clock is much more accurate than older clocks and is even more stable than others.
Redefinition of the second
Because atomic clocks are very accurate, experts are thinking about changing the way we define a second. In June 2025, scientists in six countries compared their atomic clocks. This helped them work towards creating a new global standard for measuring time using light-based atomic clocks.
Technological impact
Optical atomic clocks help make new technologies. They let people share time and frequency very accurately. This makes global navigation satellite systems even better. These clocks also help scientists measure differences in gravity and test important ideas about how our universe works.
History
The Scottish physicist James Clerk Maxwell suggested using the vibrations of light waves to measure time in 1873. He thought this would be more accurate than using the Earth's rotation.
In the 1930s, the American physicist Isidor Isaac Rabi created tools to measure the vibrations of atoms. This led to the development of atomic clocks, which are more accurate than older clocks. The first practical atomic clock, using caesium atoms, was built in the United Kingdom in 1955.
Definition of the second
Main article: Second
In 1968, scientists officially defined the second as the time it takes for a caesium-133 atom to vibrate 9192631770 times. This definition helps us keep very accurate time.
Metrology advancements and optical clocks
New technologies like lasers and optical frequency combs have made atomic clocks even more accurate. Scientists are now working on optical clocks, which use different atoms and can be even more precise. These clocks might help us redefine the second in the future.
Chip-scale atomic clocks
Scientists have also made very small atomic clocks, about the size of a grain of rice. These tiny clocks use less power and could be used in things like GPS devices.
Measuring time with atomic clocks
Clock mechanism
An atomic clock measures time by watching how atoms change energy levels. Scientists get atoms into one energy state and then shine microwave radiation on them. If the microwave has the right frequency, some atoms change to another energy state. Scientists tune the microwave to the exact frequency where the most atoms change, and use this frequency to keep very accurate time.
Unlike clocks that use the swing of a pendulum or the movement of gears, atomic clocks use the vibrations of atoms. These vibrations are not affected by temperature or other outside factors, making atomic clocks much more accurate. The frequency at which atoms vibrate is the same everywhere, making atomic clocks the most reliable way we have to measure time.
Accuracy
Atomic clocks have become more and more accurate since the first one was made in the 1950s. The earliest clocks used atoms like caesium, rubidium, and hydrogen. Scientists have made many caesium clocks that get better and better. These clocks were the first to use a caesium fountain and a method called laser cooling of atoms.
Scientists are now trying to make clocks even more accurate. They want clocks that would not lose or gain more than a second over the entire age of the universe. New types of clocks using strontium, ytterbium, and optical lattice technology are being developed. These optical clocks are more accurate because they use energy levels that vibrate faster than older atomic clocks.
Two important clocks that are very accurate are the United Kingdom's NPL-CsF2 caesium fountain clock and the United States' NIST-F2. The increase in precision from NIST-F1 to NIST-F2 was achieved by using liquid nitrogen to cool part of the clock, reducing effects from black-body radiation.
Comparing atomic clocks
Many special labs around the world keep very exact clocks called atomic clocks. These labs include places like the Paris Observatory, the National Institute of Standards and Technology in the United States, and others. They build clocks that use the vibrations of atoms to keep very accurate time.
These clocks need to be compared with each other very carefully. One way to do this is by using satellites in space. Systems like GPS, GLONASS, Galileo, and BeiDou help scientists check how well clocks match up over long distances. This is important because even tiny differences can matter.
Labs also work together to create a common time scale called International Atomic Time (TAI). This is made by averaging the time from many clocks around the world. To make everyday time match up with this, something called Coordinated Universal Time (UTC) is used. UTC adds or takes away seconds called "leap seconds" so that our clocks stay in sync with Earth's rotation.
Scientists are also finding new ways to compare clocks using special cables called fiber optics. These cables can carry time signals very accurately over long distances, helping labs check their clocks even better.
Microwave atomic clocks
Caesium
Main article: Caesium standard
Atomic clocks measure time by watching the vibrations of atoms. The official way we measure a second is based on the vibrations of caesium atoms. Caesium clocks, like the NIST-F1 clock and the NIST-F2 clock, are the most accurate timekeepers we have.
Caesium works well because it moves slower than other atoms and vibrates at a very precise frequency.
Rubidium
Main article: Rubidium standard
Rubidium atomic clocks are cheaper and smaller than caesium clocks. They are often used in portable devices and space tools. These clocks can last over ten years and cost much less. Some use signals from global positioning system to stay very accurate.
Hydrogen
Main article: Hydrogen maser
Hydrogen clocks change very little over short times, making them great for radio astronomy. However, they need regular checks to stay accurate. They are also used to test ideas about space and gravity.
Other types of atomic clocks
Nuclear clock concept
Main article: Nuclear clock
Scientists have thought about a new kind of clock called a nuclear clock. These clocks would look at changes in the heart of the atom, called the nucleus. One special type of thorium, written as 229mTh, could help make such a clock. This thorium has a low energy change that we can measure.
Researchers have measured this energy change very exactly. This means we could now build a working nuclear clock. A big benefit of a nuclear clock is that it could be more exact than today’s best clocks. The nucleus is tiny and protected, so outside forces would not affect it as much. Many atoms could also be used together, making the clock even better.
Potential for redefining the second
In 2022, the best way to measure a second uses special clocks called caesium primary standard clocks. These clocks cool a group of caesium atoms and measure how they react to certain types of light. These clocks are very accurate.
Future clocks might use light with much higher frequencies, which could make our time measurements even more precise. Scientists are also looking at ways to define the second using the properties of atoms, but this is very difficult and needs more research.
| Type | Working frequency (Hz) | Relative Allan deviation (typical clocks) |
|---|---|---|
| 133Cs | 9.192631770×109 by definition | 10−13 |
| 87Rb | 6.834682610904324×109 | 10−12 |
| 1H | 1.4204057517667×109 | 10−15 |
| Optical clock (87Sr) | 4.292280042298734×1014 | 10−17 |
| Optical clock (27Al+) | 1.12101539320785916×1015 | 10−18 |
| Optical clock (171Yb+, 642 THz) | 6.4212149677264512×1014 | 10−18 |
| Optical clock (171Yb+, 688 THz) | 6.8835897930930824×1014 | 10−16 |
Applications
Atomic clocks help us in many ways, such as in navigation satellite systems. These systems use atomic clocks to give very accurate timing signals. For example, the Global Positioning System (GPS), run by the United States Space Force, uses atomic clocks on its satellites to help us find our way.
Atomic clocks are also used in time signal radio transmitters. These clocks help make sure that time is kept very accurate for many things, like in science and for keeping records in financial systems.
Atomic clocks are also used to test ideas in science, like how time changes in different places because of gravity, as described in general relativity. Scientists use these clocks to check how accurate these ideas are.
Manufacturers
Some companies make atomic clocks that help keep the world's time. These include Microchip, T4Science, Anritsu, Microsemi, and HP. These clocks are important for keeping our time very accurate.
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