The science of surfing: A simple introduction to catching waves! (2025)

by Chris Woodford. Last updated: October 31, 2022.

Surfing is a cool way to spend a hotday—but there's much more to riding waves than just balancing on a board.Mastering surfing is all about mastering science: you need toknow how waves travel across the ocean carrying energyas theygo, and how you can capture some of this energy to move yourself along.Whether you're surfing or bodyboarding, riding a longboard or whizzingon a skimboard, you're using cool science in a very cool way. Let's take a closer look!

Photo: A surfer pulls off a 360° spin. during the US Open of Surfing.Photo by Adam Eggers courtesy of US Coastguard andDVIDS.

What are waves?

Waves are always the first thing you noticeabout the ocean.Except on very calm days, there are always waves skimming across thesurfaceof the sea. What exactly are they doing there? We usually find waves ina place where energy has appeared. A basic law of physics called theconservation of energy says that energy can'tbe created or destroyed; it can only ever be converted into other forms. When energy suddenly appears,concentrated in one place, something has to happen to it. Usually,energy doesn't stay put: it tends to travel out in all directions toother places that don't have as much.

Picture: Energy likes to travel outwards! In that respect, the waves you see riding the oceanare no different from the ripples you make in a washbasin when you let single drops hit the water surface(which is what I'm doing here).

Think about a couple of familiar examples. Suppose you bang akettle drum in the middle of a football stadium. As your arm beats thestick, you make the drum skin vibrate up and down with kinetic energy(the energy of movement). As the drum skin bounces back and forth, itproduces waves of sound energy. These travel through the air, makingair molecules vibrate in sympathy, carrying sound energy in alldirections until it dissipates and gradually disappears. Somethingsimilar happens if you switch on a lamp in the middle of a dark room.This time, waves of light energy travel out from the lamp in alldirections. Why can't you see sound and lighttraveling in the same way that you can see waves on the ocean? Soundtravels at over 1000 km/h (600 mph)—so it is both quick and invisible.Lighttravels much faster than sound at 300,000 km per second (186,000 milesper second)—soit carries electromagnetic energy betweentwo places virtuallyinstantaneously. Even though you can see light, you cannot see ittraveling.

Photo: The breaking wave behind this surfer provides all the kinetic energy that drives him forward. No waves, no energy, no surfing! Photo of surfer at Del Mar Beach Resort, California byDylan Chagnon courtesy of US Marine Corps and DVIDS.

The great thing about ocean waves is that you can see them coming.If you're surfing, even fast-moving waves are slow enough to catch andcarry you along. Try doing that with sound or light! The properties ofan ocean wave are also very easy to see. You can estimate its amplitude(height) just by looking out to the horizon. Its wavelength(the distance from one wave crest to the next) and frequency(the number of waves that travel past in a certain amount of time) arealso very easy to see.

If sound waves come from people beating drums, and light waves comefrom people switching on lamps, where do ocean waves come from? If youlive in the northern hemisphere, far from the equator, you've probablynoticed that there are more waves around in the fall (autumn) or spring thanin the summer. In the UK, for example, there's most wind in the falland winter—and that's usually the best time of year for surfing inplaces like Cornwall. Wind is important because it's what puts energyinto the ocean: it makes ocean waves in more or less exactly the sameway as you make sound waves when you bang the skin of a drum.

What's the difference between wind swell and groundswell?

The waves that arrive at your beach are not necessarily createdanywhere nearby. Back in the 1950s, an ocean scientist namedWalterMunk conducted an amazing series of experiments with ocean waves. Hemanaged to prove that some waves travel over 15,000 km (over 9000miles) across the open ocean before they reach their eventualdestination. [1]That's like traveling across the United States, from New York City to California, four times!Generally, the more widely spaced and the cleaner wavesare when they roll up on the shore, the further they have traveled.

Waves like this are known as swell (or groundswell) andthey make the best waves for surfing. Groundswell is the reason you canhave quite large waves washing up on your beach even when there'slittle or no wind blowing. Waves generated nearby (by winds blowing inthe local area) are known as wind swell.They are usuallychoppier, smaller, messier, harder to surf, and less interesting tosurfers than groundswell. Often the waves in a particular place are amixture of groundswell and wind swell—a random collection of waves thathave traveled from far away mixed with waves that have come a muchshorter distance.

Photo: Small groundswell rolling in.Note how the waves are almost evenly spaced. The distance between onewave crestand the one following is the wavelength of the wave.These waves have a wavelength of about 15 meters (50 ft).

Why is groundswell cleaner than windswell?When the wind blows on the sea, it produces all kinds of waves ofdifferent wavelengths, frequencies,and speeds.As the waves travel, the faster waves gradually separate out from theslower waves.The further the waves go, the more chance they have to sort themselvesinto an orderly pattern. Groundswell has more time to get itself intoshape than windswell.Eventually, the waves form into distinct little groups called sets:when they finally arrive at their destination, a little group of goodwaves will arrive at once.Then there will be a pause.Then the next group of waves will arrive a bit later.

When and why do waves break?

Swell is only one of the ingredients for great surfing.Surfers don't like any old waves: they want waves that peel(break gradually to the left or right along the wave crest) rather thanclose out (where the crest folds over andsmashes to pieces all in one go).When a wave is peeling, you can ride back and forth across the crest asit slowly breaks;with a wave that's closing out, there's nowhere much to go.In surfing slang, waves that close to the right are called, notsurprisingly, "righthanders",while left-breaking waves are "lefthanders".The angle at which the wave peels makes it more or less interesting tosurf. The steeper the angle, the harder it is to surf and the moreinteresting moves you can pull.

Photo: Cross-purposes: This lefthand wave is moving in the direction of the red arrow but peeling in the direction of the blue arrow; so the surfer is moving almost at a right angle to the wave, as seen from overhead.Photo of surfer in Montecito, California by Carol M. Highsmith, courtesy of The Jon B. Lovelace Collection of California Photographs in Carol M. Highsmith's America Project, Library of Congress, Prints and Photographs Division.

What makes a wave break... and peel rather than closing out?When water flows, in the ocean or in a river, its upper layers aretraveling faster than its lower layers (indeed, the water is usuallystationary on the ocean floor or on a river bed). Think about wavesarriving at a beach. As they travel fromthe open ocean to the shore, they move up a gradual sandy incline, andstart to slow down. The bottom of a wave slows morequickly than the top. So instead of a wave moving forwards as one, wehave a wholeseries of water layers sliding past one another, with the top layersmoving fastestand the bottom moving slowest.A wave breaks when the top part of the wave goes so far over the bottompart that the wavecan no longer support itself—so it completely collapses.A wave peels when this process happens gradually along the length ofthe wave rather than all at once. If you like, a peeling wave isbreaking in two dimensions: along the crest of the wave as the waveadvances up the beech or reef.

Photo: Two people surfing a peeling wave in Santa Cruz, California. A peeling wave breaks slowly and gradually along its length inside of "closing out" or "dumping" (where the whole length of the wave breaks in one go). Photo by Carol M. Highsmith, The Jon B. Lovelace Collection of California Photographs in Carol M. Highsmith's America Project, Library of Congress, Prints and Photographs Division..

Waves can break in many different ways, and that largely depends on the profile of the seabedunderneath them (known as the bathymetry).All waves will break eventually, but major features like rock or coralreefs, ledges,and sandbars will make one side break before another, causing waves topeel. Nearby groins (sea fences), piers, and jetties can also makewaves peel. Different shapes of reef produce different breakingeffects.Over the last few decades, surf science has become advanced enough forengineers to start designing artificial reefs.Rocks or ballast are buried at a key point offshore to give the waves ahelping hand in breaking and peeling early in places where they might otherwisesimply close out.

Swell and bathymetry are not the only things that affect the qualityof yoursurfing. How the wind is blowing on your beach will make a bigdifference too. Waves are obviously always traveling from the openocean towards the beach, like scaled-up versions of ripples on a pond,but the wind can be blowing in any direction. If the wind is blowingdirectly out to sea, it is known as an offshorewind. As itblows, it will naturally tend to prop up the waves, stopping them frombreaking so quickly, cleaning out some of the smaller choppierwaves, and making the waves finally break with greater intensity inshallower water.A combination of strong ground swell and a light offshore wind isalwaysbest for surfing, especially if the wind has been blowing for a fewdays (both to create groundswell and to give it time to travel to yourbeach).If the wind blows in the opposite direction, so it is onshore,it will make the waves collapse much too soon—spoiling your fun!A strong wind that is blowing directly onshore (at right angles to the beach)can produce a very random, choppy sea that is impossible to surf, but funto mess about in with a bodyboard.

Why do you have to paddle?

Science (and physics in particular) can explain most of the strangethings you'll notice when you're riding along on your surfboard.Questions like why you have to paddle...

Photo: This surfer is paddling like mad with his arms to gain speed.When the huge wave catches him up, he'll have enough momentum to leap to his feet and surf.

Whether you're on a surfboard or a bodyboard, if a great wave isheading towards you, you have to paddle like mad to be able to catchit. In other words, you have to be traveling with some speed andmomentum as the wave hits you to stand any chance of riding along with it. Whyis that? To travel with a wave, you have to accelerate to the speedit's traveling. In other words, you have to gain a certain amount ofkinetic energy very quickly. If you've already got some kinetic energyto startwith—if you're already moving when the wave catches up with you—it'smuch easier for the wave to accelerate you a little bit more. Or insimple terms, the faster you paddle, the more likely you are to catchyour wave.

Photo: If you want to catch waves on a bodyboard, fins like these are essential: by kicking with fins, you can accelerate your body much faster and greatly improve your chance of catching waves. However, it cuts both ways: once you've caught a wave, you need to lift your fins clear of the water to stop them acting like brakes and slowing you down!

Why can small kids ride small waves?

Have you noticed how young kids can ride almost any waves—but olderones can't? It's back to momentum again. To move you forward, a wave has to give you a certain amount ofmomentum and energy. Both of these depend on your mass (how much "stuff" your body is madefrom). The bigger you are, the more energy you need to travel at a certainspeed. So the older and bigger you are, the bigger the waves you need forsurfing—because bigger waves can supply you with more energy.If you're younger or smaller, you need less energy to move at thesame speed, so a smaller wave will do the job.

Why do waves suck you backwards?

At school you learn about two kinds of wave. There are waves likesound, which travel by a sort of push-pull process, making patterns ofalternately squeezed up dense air (compressions) and thinned-out,less-dense air (rarefactions). Sounds wave are called compressionwaves; they're also called longitudinal waves,because theair molecules that carry sound energy move in the same direction as thewave travels. Then there are waves like light that travel in afamiliar, up-and-down pattern. These are known as transversewaves,because they vibrate at right angles to the direction in which the wavetravels.

But ocean waves are not like the waves you learn about at school.They move the water surface round in circles as they travel along.Watch a seagull sitting on the ocean as a wave approaches. The gull issucked backwards up the front of the wave, lifted onto the wave'screst, pushed forward asthe crest passes by, and then lowered down to pretty much the sameplaceit started off in. This happens because ocean wave energy is nottraveling purely on the surface of the ocean: it also affects thelayers of water underneath. You'll have noticed this sucking effect ifyou've ever caught waves on a bodyboard. As you lie on the sea surface,you'll feel yourself being pulled backwards as a wave approaches. Thisis another reason why you have to be paddling forwards to catch a wave.If you're not paddling forwards, you're definitely going to get suckedbackwards!

Photo: Layers of water slide pastone another at the shore. At the top of the beach, water is suckingback down into the sea.Just offshore, a small wave is breaking inwards and up the beach. Inbetween, another small wave has just broken and is coming to a halt.There are at least three layers of water sliding over one another here.In these calm conditions, the liquid layers are moving in what physicistswould call laminar flow.

Why does a surfboard have a curved front edge?

Photo: The curved front edge of my Manta bodyboard. If I lay this board down on a flat floor, ithas a very noticeable—amost banana-like—curve to it.

Everything from the biggest ocean liner to the smallest surfboardhas a curved front edge. Why? If you push a curved edge over water, thecurve makes water travel more quickly underneath than on top. Thisgenerates an upward force called lift that moves you up and slightlyout of the water—an effect called planing. Because you're partlyout of the water, there's less drag (water resistance) and you gofaster. You can see planing happening on almost any boat as it picks upa bit of speed. With a hydrofoil—a kind of "surfing boat"—the planing is so spectacularthat the entire craft lifts up out of the water. The same science is atwork on a surfboard, only not quite so dramatic!

What about tides?

Tides have nothing to do with waves. Tides are caused by the Moonand the Sun working together to "pull" the sea back and forth withtheir gravity, rather like a giant blanket moving up and down a bed. Tides change the depthof the water on your beach. When the tide is "in", the waves come infurther and break later; when the tide is "out", the waves breakfurther out. Depending on the profile of the seabed, a rising tide (onecoming in) or a falling tide (one going out) will make the waves tendto break somewhat better or somewhat worse than usual, depending on the local seabed. There is no absolute rule that works everywhere: some places work well as high tide approaches; somework best when the tide is going out.

Photo: Low tide with offshore wind and a small groundswell. Even if you could catch "waves" this small,science tells us they have too little energy to take you anywhere. This water's definitely not for surfing, but you might get a few short rides on your boogie board if you're really lucky. Not that it matters. These guys are having more fun in the waterthan I am taking their photo: the number one rule of surfing is that there's always more fun in the water than watching from the beach.

When the Moon and Sun line up, twice a month, they make higher tides than usualcalled spring tides, which give deeper waterduring high tides(when the tide is in) and shallower water at low tide (when the tide isout). In between the spring tides are neap tides,when the sea movesback and forth less than usual, high tides are less deep, and low tidesare less shallow. Again, depending on the seabed, high and low tides,and spring and neap tides, will make the surfing better orworse—but it varies wildly from place to place. If you're in a placethat needs deep water to make the waves break properly, the highestspring tides are going to be better than the lowest neap tides. Butelsewhere, the opposite may be true.

Why wear a wetsuit?

The synthetic rubber traps water next to your body, which provides auseful layer of insulation to keep you warm.Read our article about wetsuits to find out more.

Can science make you a better surfer?

Of course! It won't make you stand on the board any better. But ifyou understand what waves are, how they are made, and where they comefrom, you'll have a much better idea of when the surf's going to be up.And if you can predict when the waves are ready to ride,you're halfway there already. If surfing is a quest for the perfectwave, science can at least point you in the right direction.It might not make you a better surfer, but itcertainly won't make you any worse!

Who invented the surfboard?

Modern surfing evolved during the late-19th and early-20th centuries, and it's not possible to identifya single inventor of either surfing or surfboards. Surfing is certainly much older than most people believe:the earliest photo of surfing I can find on the US Library of Congress website was taken in Hawaii sometime between 1906 and 1916,and accounts from missionaires there (who strongly discouraged what they called a "heathen sport") date it back to at least the early 19th century. [2] One person who does merit a mention is American surfer Tom Blake (1902–1994), who pioneered all sorts of improvements in boards between the mid-1920s and mid-1930s. In 1932, he patented the hollow, internally braced wooden surfboard, which was the forerunner of modern laminated and composite boards). Blake described his invention as "especially adaptable for swimmers or bathers, whereby they may be efficiently floated on the water and may propel the device with the hands and arms through the water at a very rapid speed and obviate the employment of oars or paddles,"making a fun form of recreation that was "simple, durable and efficient and which may be manufactured and sold at a comparatively low cost." The development of affordable, lightweight, easy-to-manufacture surfboards, along with other innovations like the invention of wetsuits, helped to turn surfing into the major international sport we know today.

Artwork: A sketch of Tom Blake's hollow, internally reinforced surfboard from his US Patent: 1,872,230: Water Sled, with colors added for clarity by me, courtesy of US Patent and Trademark Office. The internal skeleton of the board is colored red. As Blake's patent notes, the main advantages are this design are high buoyancy, low weight, and low cost.

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On this website

• Science of sport
• Swimming
• Water
• Wetsuits

More surf science articles by me

A few years ago, I began work on a series of simple articles for the European Association of Surfing Doctors(now Surfing Medicine International). These are archived from the Wayback Machine:

• The Energy in Waves (July 2015). Explores where waves get their energy from, what makes the biggest waves, and estimates how much useful energy there is in a wave.
• The Wonder of Wetsuits (December 2012). Why do we need wetsuits for cold-water surfing? How do they work? Who invented them?

On other websites

• The Science of Surfing Waves: A more technical review from scientists at Scripps Institution of Oceanography.
• Waves: A great guide to basic wave physics from the University of Salford (including lots of easy-to-understand animations). This site is mainly about sound waves, but a lot of the same physics applies to ocean waves.

Books

Wave science

• Surf Science by Tony Butt. Honolulu, Hawaii: University of Hawaii Press, 2014. This is a very clear, simple introduction to wave and surf science, well illustrated with good color illustrations and photos.
• The Surfer's Guide to Waves, Coasts, and Climates by Tony Butt. Alison Hodge, 2009. A more general look at waves than you'll find in Tony's Surf Science book.

Oceanography

• Essentials of Oceanography by Alan P. Trujillo and Harold V. Thurman. Prentice Hall, 2016. A very readable introductory textbook on oceanography and marine science. A good starting point if you want to know how the oceans work. This was the book that kick-started my interest in ocean science some years ago. Chapter 8, "Waves and Water Dynamics", is a good introduction to why waves are formed and how they travel.
• The Wave Watcher's Companion: Ocean Waves, Stadium Waves, and All the Rest of Life's Undulations by Gavin Pretor-Pinney. Penguin Group USA, 2011. A very readable look into all the ways in which waves ripple through our lives. There's quite a bit about ocean waves and surfing, but lots of other wave topics get a mention too (in other words, it's not just about surfing).
• Waves, Tides and Shallow-Water Processes by John Wright, Angela Colling, and Dave Park. Butterworth-Heinemann/Open University, 1999. A more general look at water movements near the shore.
• Waves and Beaches: The Dynamics of the Ocean Surface by Willard Bascom. Doubleday, 1954 (and later editions). A classic of oceanography, this book inspired many of the later books about wave dynamics. Although long out of print, it's relatively easy to find secondhand copies. An excellent short article summarizing the main ideas was published as "Ocean Waves" in Scientific American, August 1959.

Surfing history and culture

• The Book of Surfing by Michael Fordham. London: Harper, 2012. A great, coffee-table introduction to surf-culture. Not much about surf science, but that doesn't matter.
• The History of Surfing by Matt Warshaw.Chronicle Books, 2011. A lavishly illustrated chronology from late-19th-century beginnings to the most recent innovations.There's also a shorterA Brief History of Surfing by Matt Warshaw.Chronicle Books, 2017, which is abut half the length.
• The Encyclopedia of Surfing by Matt Warshaw.Houghton Mifflin Harcourt, 2005. A more general, more comprehensive, old-school encyclopedia. A–Z entries cover everything from surf terminology ("cutback," "deck patch") to history and culture, with many biographies of key surfers, and lots of information about famous surf spots around the world.

Practical guides

• Surfing Manual: The Essential Guide to Surfing in the UK and Abroad by Peter Carr. Haynes, 2017. A well-illustrated guide, but quite UK-centric.
• Surfing: A Beginner's Guide by Alf Alderson. Wiley, 2008. A comprehensive guide to the fundaments of surfing—water safety, equipment, fitness, where to surf around the world, and more.

1. ↑Surf Science by Tony Butt and Paul Russell. Honolulu, Hawaii: University of Hawaii Press, 2002, p.39–41. by Patrick Moser, The Journal of the Polynesian Society, Vol. 125, No. 4, Dec 2016, pp.411–432.
2. ↑The endurance of surfing in 19th-century Hawai'i byPatrick Moser, The Journal of the Polynesian Society, Vol. 125, No. 4, Dec 2016, pp.411–432.