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Sound—it’s almost impossible to imagine a world without it. It’s probably the first thing you experience when you wake up in the morning—when you hear birds chirping or your alarm clock bleeping away. Sound fills our days with excitement and meaning, when people talk to us, when we listen to music, or when we hear interesting programs on the radio and TV. Sound may be the last thing you hear at night as well when you listen to your heartbeat and drift gradually into the soundless world of sleep. Sound is fascinating—let’s take a closer look at how it works!

What is sound?

Sound is the energy things produce when they vibrate (move back and forth quickly). If you bang a drum, you make the tight skin vibrate at very high speed (it’s so fast that you can’t usually see it), forcing the air all around it to vibrate as well. As the air moves, it carries energy out from the drum in all directions. Eventually, even the air inside your ears starts vibrating—and that’s when you begin to perceive the vibrating drum as a sound. In short, there are two different aspects to sound: there’s a physical process that produces sound energy to start with and sends it shooting through the air, and there’s a separate psychological process that happens inside our ears and brains, which convert the incoming sound energy into sensations we interpret as noises, speech, and music. We’re just going to concentrate on the physical aspects of sound in this article.

Sound is like light in some ways: it travels out from a definite source (such as an instrument or a noisy machine), just as light travels out from the Sun or a light bulb. But there are some very important differences between light and sound as well. We know light can travel through a vacuum because sunlight has to race through the vacuum of space to reach us on Earth. Sound, however, cannot travel through a vacuum: it always has to have something to travel through (known as a medium), such as air, water, glass, or metal.

The first person to discover that sound needs a medium was a brilliant English scientist known as Robert Boyle (1627–1691). He carried out a classic experiment that you’ve probably done yourself in school: he set an alarm clock ringing, placed it inside a large glass jar, and while the clock was still ringing, sucked all the air out with a pump. As the air gradually disappeared, the sound died out because there was nothing left in the jar for it to travel through.

Robert Boyle’s classic experiment


  1. Put a ringing alarm clock inside a large glass case with a valve on top. Close the valve so no air can get in.
  2. You can easily hear the clock ringing because the sound travels through the air in the case and the glass, before continuing to your ears.
  3. Switch on the vacuum pump and remove the air from the case. As the case empties, the ringing clock sounds fainter and fainter until you can barely hear it at all. With little or no air in the case, there’s nothing to carry the sound to your ears.
  4. Switch off the pump. With the clock still ringing, open the valve on top of the case. As air rushes back in, you’ll hear the clock ringing once again. Why? Because with air once again inside the case, there’s a medium to carry the sound waves from the ringing clock to your ears.

How sound travels?

When you hear an alarm clock ringing, you’re listening to energy making a journey. It sets off from somewhere inside the clock, travels through the air, and arrives some time later in your ears. It’s a little bit like waves traveling over the sea: they start out from a place where the wind is blowing on the water (the original source of the energy, like the bell or buzzer inside your alarm clock), travel over the ocean surface (that’s the medium that allows the waves to travel), and eventually wash up on the beach (similar to sounds entering your ears). If you want to learn more about how sea waves travel, read our article on surfing science.

A line artwork comparing longitudinal sound waves and transverse ocean waves.

There is one crucially important difference between waves bumping over the sea and the sound waves that reach our ears. Sea waves travel as up-and-down vibrations: the water moves up and down (without really moving anywhere) as the energy in the wave travels forward. Waves like this are called transverse waves. That just means the water vibrates at right angles to the direction in which the wave travels. Sound waves work in a completely different way. As a sound wave moves forward, it makes the air bunch together in some places and spread out in others. This creates an alternating pattern of squashed-together areas (known as compressions) and stretched-out areas (known as a rarefactions). In other words, sound pushes and pulls the air back and forth where water shakes it up and down. Water waves shake energy over the surface of the sea, while sound waves thump energy through the body of the air. Sound waves are compression waves. They’re also called longitudinal waves because the air vibrates along the same direction as the wave travels.

The science of sound waves

If you’ve ever got time on your hands while you’re lazing on the beach, try watching the different ways in which waves can behave. You’ll notice that waves traveling on water can do all kinds of clever things, like smashing into a wall and reflecting straight back with more or less the same intensity. They can also spread out in ripples, creep their way up the beach, and do other clever stuff. What’s happening here with water waves doesn’t actually have anything to do with the water: it’s simply the way energy behaves when it’s carried along by waves. Similar things happen with other kinds of waves—with light and with sound too.

You can reflect a sound wave off something the same way light will reflect off a mirror or water waves will bounce off a sea wall and go back out to sea. Stand some distance from a large flat wall and clap your hands repeatedly. Almost immediately you’ll hear a ghostly repeat of your clapping, slightly out of step with it. What you hear is, of course, sound reflection, better known as an echo: it’s the sound energy in your clap traveling out to the wall, bouncing back, and eventually entering your ears. There’s a delay between the sound and the echo because it takes time for the sound to race to the wall and back (the bigger the distance, the longer the delay).

Side-scan sonar image of a World War II patrol boat on the seabed.

Picture: Reflected sound is extremely useful for “seeing” underwater where light doesn’t really travel—that’s the basic idea behind sonar. Here’s a side-scan sonar (reflected sound) image of a World War II boat wrecked on the seabed. Photo courtesy of U.S. National Oceanographic and Atmospheric Administration and US Navy.

Sound waves lose energy as they travel. That’s why we can only hear things so far and why sounds travel less well on blustery days (when the wind dissipates their energy) than on calm ones. Much the same thing happens on the oceans. Crisp water waves can sometimes travel vast distances across the ocean, but they can also be messed up when squally weather dissipates their energy over shorter distances.

Sound waves are like light and water waves in other ways too. When water waves traveling long distances across the ocean flow around a headland or into a bay, they spread out in circles like ripples. Sound waves do exactly the same thing, which is why we can hear around corners. Imagine you’re sitting in a room off a corridor and, much further up the corridor, there’s an identical room where someone is practicing a trumpet inside. Sound waves travel out from the trumpet, spreading out as they go. They ripple out down the corridor, race along it, ripple through the doorway into your room and eventually reach your ears. The tendency waves have to spread out as they travel and bend around corners is called diffraction.

Whispering galleries and amphitheaters

US Capitol dome

US marines sitting in an amphitheater in Iraq

You might not think you could hear someone whispering if they sat a long way away, but if they can make the sound of their voice bounce off something into your ears, their voice will travel much further than usual.

If you’re inside a building with a giant dome, the sounds you make will reflect off the curved roof like light rays bouncing off a mirror. Buildings that work this way are sometimes called whispering galleries. The dome of the US Capitol and the famous reading room in the British Museum in London are two well known examples. You can hear the same effect at work outside when you sit in a naturally curved area called an amphitheater. You can talk in a normal voice and still be heard very clearly a considerable distance away.

Photos: Left: The Capitol in Washington, DC has a whispering gallery inside its dome. Photo by courtesy of The Architect of the Capitol. Right: It’s easy to hear people talking in this amphitheater in Iraq. Photo by Jason L. Andrade courtesy of US Marine Corps and Defense Imagery.

How Sound Works?

Step 1: What sound is/air movement


Sound travels in waves.  Almost all sounds can be created from, or reduced to a sine wave.  You can see a very deep sine wave in the picture.

Sound is the movement of air.  When you hear something, parts of your ear are vibrating.  When you speak, your voice causes air to move, which causes parts in your ear and other people’s ears to vibrate.  Most microphones work in a similar way to the human ear.  When sound travels across the diaphragm, it causes it to vibrate, and then convert into electricity (signal).  A speaker works in the opposite way.  When a speaker receives signal (electricity), it causes parts of the speaker to move back and forth which causes air to move.  This way, it allows you to hear the sound.

Step 2: Volume vs. pressure


When you hear something, you have to remember that volume has very little to do with how loud a sound is.  It is all about pressure (SPL).  The greater the pressure, the more the parts in your ear move, and the louder the sound is heard.  This is why having your music too loud is bad for your ears.  Your ear is like anything else in this world, it has limits.  When you have a lot of movement in your ear, your ear tries to adjust, so that it doesn’t totally destroy your ear.  It adjusts by limiting the movement/sensitivity within your ear.  Once your ear adjusts, it is very hard to undo.  Your ear adjusts in many other ways too.  If you are straining to hear a specific frequency, your mind will adjust what frequencies it wants to hear so that it encompasses what you are trying to hear.  You do not have any more or less hearing, but a different frequency range.  In this way, you are not straining your ear, but it can make it harder to hear/understand frequencies that you were able to hear/understand with no problem before.  When sound travels, the pressure decreases.  The inverse square law states that in normal conditions, as you double your distance from the source, the sound is reduced by 6 dba (4x).

Step 3: Reverberation vs. echo


Reverberation is what happens when sound bounces off something flat and hard.  Many people mistake reverberation for echo.  Reverberation is what happens when you shout and you hear Hello o o o o o o o o o etc.  Echo is when you shout and you hear Hello Hello Hello Hello Hello etc.  Many times you have problems with too much reverberation when you are in a gymnasium.  Acoustical treatments can be used to reduce reverberation.  Some times you may want to use a little reverberation to make something sound big and “booming”.  In this case, you can use digital effects to add just the right amount of reverberation.

Measuring waves

All sound waves are the same: they travel through a medium by making atoms or molecules shake back and forth. But all sound waves are different too. There are loud sounds and quiet sounds, high-pitched squeaks and low-pitched rumbles, and even two instruments playing exactly the same musical note will produce sound waves that are quite different. So what’s going on?

The energy something makes when it vibrates produces sound waves that have a definite pattern. Each wave can be big or small: big sound waves have what’s called a high amplitude or intensity and we hear them as louder sounds. Loud sounds are equivalent to larger waves moving over the sea (except that, as you’ll remember from up above, the air is moving back and forth, not up and down as the water does).

Apart from amplitude, another thing worth noting about sound waves is their pitch, also called their frequency. Soprano singers make sound waves with a high pitch, while bass singers make waves with a much lower pitch. The frequency is simply the number of waves something produces in one second. So a soprano singer produces more energy waves in one second than a bass singer and a violin makes more than a double bass.

Understanding amplitude and frequency

A simple explanation of the concepts of amplitude and frequency.

  1. The top wave represents a typical sound wave vibrating at a certain amplitude (its height) and frequency (how many peaks and troughs there are in a certain amount of time).
  2. This wave has the same frequency as the first wave (the same number of peaks and troughs) but twice the amplitude (it’s twice as high). A sound wave like this would be about twice as loud as the first wave but the same pitch.
  3. This wave has half the frequency of the second wave (half the number of peaks and troughs) but the same amplitude (it’s exactly the same height). A sound wave like this would sound deeper (lower pitched) than the second wave, about as loud as the second wave, and twice as loud as the first wave.
  4. This wave has twice the frequency of waves 1 and 2 and four times the frequency of wave 3, so it would sound much higher in pitch than the other waves. It has the same amplitude as waves 2 and 3, so it would sound just about as loud.

Remember, however, that sound waves don’t look like this as they travel. These up-and-down patterns are what you’ll see if you study sound wave signals with an oscilloscope (a kind of electronic graph-drawing machine). Sound waves travel through the air as squashed-up compressions and stretched-out rarefactions. They only look like this on an oscilloscope trace.

Why instruments sound different

But here’s a conundrum. If a violin and a piano make sound waves with the same amplitude and frequency, how come they sound so different? If the waves are identical, why don’t the two instruments sound exactly the same? The answer is that the waves aren’t identical! An instrument (or a human voice, for that matter) produces a whole mixture of different waves at the same time. There’s a basic wave with a certain amplitude and pitch, called the fundamental, and on top of that there are lots of higher-pitched sounds called harmonics or overtones. Each harmonic has a frequency that’s exactly two, three, four, or however many times higher than the fundamental. Every instrument produces a unique pattern of a fundamental frequency and harmonics, called timbre (or sound quality). All these waves add together to give a unique shape to the sound wave produced by different instruments, and that’s one reason why they sound different. The other reason is that the amplitude of the waves made by a particular instrument changes in a unique way as the seconds tick by. Flute sounds are immediate and die quickly, while piano sounds take longer to build up and die out more slowly as well. You’ll find a much longer explanation of this in our article about electronic music synthesizers.

The speed of sound

When we talk about the speed of sound, what exactly do we mean? Now you know that sound carries energy in a pattern of waves, you can see that the speed of sound means the speed at which the waves move—the speed at which the energy travels between two places. When we say that a jet airplane “breaks through the sound barrier,” we mean that it accelerates so fast that it overtakes the incredibly high-intensity (that is, noisy) sound waves its engines are making, producing a horrible noise called a sonic boom in the process. That’s why you’ll see a fighter plane whizz overhead a second or two before you hear the vicious scream of its jet engines.

Jet airplane: Condensation cloud created by a fighter jet.

Photo: Breaking through the sound barrier creates a sonic boom. The mist you can see, which is called a condensation cloud, isn’t necessarily caused by an aircraft flying supersonic: it can occur at lower speeds too. It happens because moist air condenses due to the shock waves created by the plane. You might expect the plane to compress the air as it slices through. But the shock waves it generates alternately expand and contract the air, producing both compressions and rarefactions. The rarefactions cause very low pressure and it’s these that make moisture in the air condense, producing the cloud you see here. Photo by John Gay courtesy of US Navy.

The speed of sound in air (at sea level) is about 1220 km/h (760 mph or 340 meters per second). Compared to light waves, sound waves creep along at a snail’s pace—about a million times slower. You see lightning much sooner than you hear it because the light waves reach you pretty much instantly, while the sound waves take about 5 seconds to cover each 1.6 km (1 mile).

One thing to note about the speed of sound is that there’s really no such thing! Sound travels at different speeds in solids, liquids, and gases and even its speed in one material can change. Very roughly speaking, how fast it goes varies according to the density of the medium (how much stuff there is there). It’s faster in solids than in liquids and faster in liquids than in gases: for example, sound travels about 15 times faster in steel than in air, and about four times faster in water than in air.That’s why whales use sound to communicate over such long distances and why submarines use SONAR (sound navigation and ranging; a sound-based navigation system similar to radar only using sound waves instead of radio waves). It’s also one of the reasons why it’s very hard to figure out where the noise of a boat engine is coming from if you’re swimming in the sea. (Note: The way sound travels through different materials is much more complex than this. A good explanation of why sound goes so fast in solids would mean I’d have to introduce a concept called phonons—and I’m going to skip that in this simple, introductory article, gloss over the complexities, and “pretend” that density is what makes the difference.)

Sound travels at different speeds in different gases—and can go at different speeds even in the same gas. It travels much faster in warm air near the ground than in colder air higher up, for example. And it travels roughly three times faster in helium gas than in ordinary air, because helium is much less dense. That’s why people who breathe in helium talk in funny voices: the sound waves their voices make travel faster—with higher frequency.

Sound in practice

A Steinway grand piano at Lanhydrock, Cornwall

Sound is a hugely important part of life on Earth. Most animals listen out for noises—things that signal the possibility of eating or being eaten. Many creatures also exchange meaningful sounds, either to communicate with members of the same species or warn off predators and rivals. Humans have evolved this ability into spoken language (as a way of exchanging information) and music (essentially, a sound-based system for communicating emotion).

We’ve also developed a variety of different sound technologies. We’ve invented musical instruments that can make a huge range of different musical sounds, from simple drums and percussion instruments to sophisticated electronic synthesizers that can generate any sound you care to imagine. We can record sounds on such things as compact discs or with newer technologies like MP3 (sound files stored in highly compressed forms on computers). We can also use very high frequency sounds, known as ultrasound, for everything from cleaning false teeth to studying the development of a baby inside a mother’s womb. We’ve even taught computers to listen to our spoken words and turn them into written language using voice recognition software—appropriately enough, that’s how I wrote this article for you today!

Photo (left): Musical sound is arguably humankind’s greatest invention. This superb Steinway grand piano dates from 1876 and sits in the amazing gallery at the National Trust’s Lanhydrock country house in Cornwall, England.
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